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University of Groningen
The acid gas solubility in Aqueous N-MethyldiethanolamineHuttenhuis, Patrick Johannes Gerhardus
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THE ACID GAS SOLUBILITY IN
AQUEOUS N-METHYLDIETHANOLAMINE;
EXPERIMENTS AND THERMODYNAMIC MODELLING
Patrick J.G. Huttenhuis, Hengelo, The Netherlands
The Acid Gas Solubility in Aqueous N-Methyldiethanolamine;
Experiments and Thermodynamic Modelling
PhD Thesis, University of Groningen, The Netherlands
Cover: Detail of the equilibrium reactor
Printing: Ipskamp Drukkers B.V., Enschede, The Netherlands
Copyright © 2009 Huttenhuis, P.J.G.
All rights reserved. This book, or any parts thereof, may not be reproduced in any
form without written permission from the author.
RIJKSUNIVERSITEIT GRONINGEN
THE ACID GAS SOLUBILITY IN
AQUEOUS N-METHYLDIETHANOLAMINE;
EXPERIMENTS AND THERMODYNAMIC MODELLING
Proefschrift
ter verkrijging van het doctoraat in de
Wiskunde en Natuurwetenschappen
aan de Rijksuniversiteit Groningen
op gezag van de
Rector Magnificus, dr. F. Zwarts,
in het openbaar te verdedigen op
vrijdag 19 juni 2009
om 14.45 uur
door
Patrick Johannes Gerhardus Huttenhuis
geboren op 14 juni 1970
te Oldenzaal
Promotor: Prof. dr. ir. G.F. Versteeg
Beoordelingscommissie: Prof. dr. R. Taylor
Prof. ir. J.A. Wesselingh
Prof. dr. ir. H.J. Heeres
ISBN 978-90-367-3841-5 (printed version)
ISBN 978-90-367-3840-8 (digital version)
Voor Brigitte, Tessa en Bas
en mijn ouders
vii
Summary
Acid gases are frequently present in industrial gases and have to be removed for
corrosion prevention, operational, economical and/or environmental reasons
respectively. A vast amount of commercial processes are available to deal with the
acid gas removal. Chemical absorption using an aqueous alkanolamine solvent is
the most commonly used process in the gas treating industry. In this process the
acid gas is contacted with a solvent in an absorber and, via chemical reactions,
converted to non-volatile species in the liquid. The acid gas containing solvent is
routed to a desorber, where the acid gas is released from the solvent at a higher
temperature and/or lower pressure. For the design of gas treating equipment a
reliable rate based simulation program is required, which describes the involved
complex mass transfer phenomena accurately. The thermodynamics of the acid gas
– solvent system play also a very important role in the mass transfer model. To
describe these thermodynamics an accurate thermodynamic model is required,
which has to be validated with experimental data.
In this thesis a new thermodynamic model for acid gas – alkanolamine systems has
been used and further developed. This model, based on an electrolyte equation of
state (E-EOS) was originally introduced by Fürst and Renon (Fürst, W.; Renon, H.
Representation of excess properties of electrolyte solutions using a new equation of
viii Summary
state, AIChE Journal, 39 (1993) 335-343). In this electrolyte equation of state
approach both the vapor and the liquid are described with an equation of state.
Several ionic terms needed to be added to this equation of state approach in order
to take into account the additional interactions due to the ions present in the liquid.
In this thesis the E-EOS model has been developed to study the solubility of the
acid gases carbondioxde (CO2) and hydrogensulphide (H2S) in aqueous N-
Methyldiethanolamine (MDEA) respectively. MDEA is commonly used in the gas
treating industry for selective H2S removal, but it is also used for other applications.
Initially, the E-EOS has been used to study the acid gas solubility at low total
system (atmospheric) pressures. These solubility data are available widely in the
literature. However, the pressure in an absorber of a natural gas plant is in general
significantly higher. Therefore, also new acid gas (CO2 and/or H2S) solubility data in
aqueous MDEA were determined at high partial pressure of methane (up to 69 bar).
These experimental solubility data are compared also with the E-EOS model
developed in this study.
In Chapter 2 an overview of several thermodynamic models is presented, which can
be used to describe the thermodynamics of an acid gas – alkanolamine system.
Each thermodynamic model/approach has its own specific pro and cons. At high
pressure applications (i.e. natural gas), however, an electrolyte equation of state
seems to be very attractive, due to the uniform approach of both the liquid and the
vapor phase respectively.
In Chapter 3 the electrolyte equation of state as developed by Solbraa (Solbraa, E,
Ph.D. Thesis Norwegian University of Science and Technology (2002)) was further
developed to study the solubility of CO2 in aqueous MDEA. The improved model
has been compared with solubility data for the system CO2-H2O-MDEA as
presented in the open literature. The calculated (speciated) liquid composition is
compared with speciation data (with a NMR technique) as presented in the
literature. The prediction of the speciation with the E-EOS appeared to be very well
Summary ix
in line with the NMR data. In Appendix A new CO2 solubility data in aqueous MDEA
are presented at different liquid loadings (0.047 – 1.105 mol.mol-1
), temperatures
(283 and 298 K), MDEA concentrations (35 and 50 wt.%) and partial pressures of
methane (up to 69 bar). It has been demonstrated (experimentally and by E-EOS)
that both the system pressure and/or partial pressure of methane have a significant
effect on the solubility of CO2 in aqueous MDEA solutions respectively. A decrease
in CO2 solubility has been observed, when the partial pressure of methane is
increased. It is concluded from E-EOS simulations that this decreasing solubility is
caused by a lowering of the CO2 fugacity coefficient at increasing methane partial
pressure.
In Chapter 4 the electrolyte equation of state as described in Chapter 3 is further
extended to calculate the solubility of H2S in aqueous MDEA. Several, H2S specific
pure component and binary interaction parameters have been included in the E-
EOS. The model has been validated with solubility data of H2S in aqueous MDEA in
the absence and the presence of methane as a make-up gas respectively. In
Appendix A new H2S solubility data in aqueous MDEA are presented at different
liquid loadings (0.028 – 0.075 mol.mol-1
), temperatures (283 and 298 K), MDEA
concentration (35 and 50 wt.%) and partial pressures of methane (up to 69 bar). For
both the system H2S-MDEA-H2O and H2S-MDEA-H2O-CH4 the model under-
predicts the acid gas partial pressure (and over-predicts the acid gas solubility).
However, model predictions for the system in absence of methane are much more
in agreement with the experimental data. Both experimental data and model
calculations show that an increase in partial pressure of methane results in a
decrease of H2S solubility. It is concluded from E-EOS simulations that this
decreasing solubility is caused by a decreasing H2S fugacity coefficient at
increasing methane partial pressure.
In Chapter 5 the solubilities of CO2 and H2S, when present simultaneously in
aqueous MDEA, have been studied experimentally and theoretically. This is with
x Summary
and without methane acting as inert component. New datapoints are presented for
35 and 50 wt.% aqueous MDEA at 283 and 298 K and several liquid loadings. The
methane partial pressure has been varied from 6.9 up to 69 bar. The H2S partial
pressure increases significantly with the CO2 liquid loading, i.e. the capacity of the
solvent for H2S capture decreases. The experimental results are compared to the
electrolyte equation of state as developed for single gas systems in Chapter 3 and 4
of this thesis. When CO2 and H2S are present simultaneously, only one additional
new parameter is required compared with the two single gas E-EOS modules. Only
the value of the CO2-H2S molecular interaction parameter needs to be determined.
During simulations with the E-EOS it appeared that the model results were hardly
sensitive to the value of this parameter. Initially, the E-EOS was compared with
solubility data in open literature for the system CO2-H2S-MDEA-H2O. In general it
can be concluded that the E-EOS is able to predict the simultaneously solubility of
CO2 and H2S in aqueous MDEA satisfactorily. The E-EOS model is also compared
to the experimental data of the CO2-H2S-MDEA-H2O-CH4 system as presented in
Chapter 5. The model is also able to predict these experimental results with good
agreement.
Based on the results as described in this thesis, it is concluded that the electrolyte
equation of state (E-EOS) approach gives very promising results for the prediction
of the thermodynamics of acid gas – alkanolamine systems. It has been proven that
the model can be extended from binary non-reactive systems, to reactive single gas
systems (CO2 and H2S) and to reactive systems, where these acid gases are
present simultaneously. It is expected that the model can be improved significantly,
when more experimental physical and chemical equilibrium data are available. For
example the following data are scarce in the (gas treating) literature:
• Binary thermodynamic data
VLE, heat of mixing, etc of binary water – alkanolamine systems;
Summary xi
• Speciation data of the reactive acid gas – alkanolamine system
At the moment the several ionic interaction parameters are determined from
total acid gas solubility data. However, these parameters can be determined
more accurately, when the concentration of the several molecular and ionic
species in the liquid is known. When these speciation data are available,
the molecular CO2 concentration does not have to be estimated from the
CO2-N2O analogy as done in this thesis, but can be determined directly;
• Thermodynamic data at high (methane partial) pressure
In general the thermodynamic data are determined during low
(atmospheric) pressure. However, in this thesis it has been proven that the
(methane partial) pressure plays an important role on the acid gas solubility.
Substantially more research is also required in this area to study the
influence of other inert components, such as nitrogen, oxygen and other
hydrocarbons on the acid gas solubility in aqueous alkanolamine solutions.
xii Summary
xiii
Samenvatting
Zure gassen zijn veelvuldig aanwezig in verschillende concentraties in industriële
gassen. Deze moeten vaak verwijderd worden vanwege corrosie preventie,
operationele, economische en/of milieu aspecten. Er bestaan verschillende
commerciële processes om deze zure gassen te verwijderen. Chemische absorptie
met behulp van een waterige alkanolamine oplossing in water is het meest
gebruikte proces in de gas behandelings industrie. Tijdens dit proces wordt het zure
gas in contact gebracht met een oplosmiddel in een absorptie kolom en omgezet in
niet vluchtige componenten. Vervolgens wordt het oplosmiddel met het
gereageerde zure gas naar een desorptie kolom geleid. In deze desorber worden
de zure gassen weer vrij gemaakt door het verhogen van de temperatuur en/of het
verlagen van de druk. Voor het ontwerp van een gas behandelings installatie is een
betrouwbaar simulatie programma nodig, waarin alle complexe stof overdrachts
verschijnselen worden meegenomen. De thermodynamica van het zure gas –
oplosmiddel systeem speelt een belangrijke rol in het stof overdrachts model. Deze
thermodynamica kan beschreven worden met een thermodynamisch model, dat
gevalideerd moet worden met experimentele data.
In dit proefschrift wordt een nieuw model gebruikt en verder ontwikkeld om de
thermodynamica van zuur gas – alkanolamine systemen te beschrijven. Dit model is
gebaseerd op een “electrolyte equation of state” (E-EOS), welke geïntroduceerd is
xiv Samenvatting
door Fürst and Renon (Fürst, W.; Renon, H. Representation of excess properties of
electrolyte solutions using a new equation of state, AIChE Journal, 39 (1993) 335-
343). In deze “electrolyte equation of state” worden zowel de gas- als de
vloeistoffase beschreven met behulp van dezelfde toestandsvergelijking.
Verschillende termen die de aanwezigheid van ionen beschrijven zijn vervolgens
toegevoegd aan deze toestandsvergelijking. In dit proefschrift is een model
ontwikkeld dat de oplosbaarheid van de zure gassen koolstofdioxide (CO2) en
waterstofsulfide (H2S) in een waterige N-Methyldiethanolamine (MDEA) oplossing
kan beschrijven. MDEA wordt veelvuldig gebruikt in de gas behandelings industrie
om o.a. H2S selectief te verwijderen. In eerste instantie is het E-EOS model gebruikt
om de oplosbaarheid van zure gassen te bestuderen bij een lage (atmospherische)
druk. Deze oplosbaarheids data zijn veelvuldig aanwezig in de literatuur. Echter, de
druk in de absorptie kolom van een aardgas installatie is in het algemeen veel
hoger. Daarom zijn er in dit proefschrift nieuwe oplosbaarheids data gepresenteerd
(CO2 en/of H2S in een waterige MDEA oplossing) bij hoge methaan partiaal drukken
(tot 69 bar). Deze oplosbaarheidsdata zijn vergeleken met simulatie resultaten van
het E-EOS model.
In hoofdstuk 2 is een overzicht gegeven van verschillende thermodynamische
modellen welke gebruikt kunnen worden om de thermodynamica van zure gas –
alkanolamine systemen te beschrijven. Elk thermodynamisch model heeft zijn voor-
en nadelen. Voor hoge druk applicaties (b.v. aardgas behandeling) lijkt een
“electrolyte equation of state” aantrekkelijk, omdat zowel de gas- als vloeistoffase
op dezelfde manier worden beschreven worden.
In hoofdstuk 3 is de door Solbraa (Solbraa, E, proefschrift Norwegian University of
Science and Technology (2002)) ontwikkelde “electrolyte equation of state” verder
ontwikkeld om de oplosbaarheid van CO2 in een waterige MDEA oplossing te
bestuderen. Het verbeterde model is vergeleken met oplosbaarheidsdata van het
systeem CO2-H2O-MDEA zoals die bekend zijn in de literatuur. De berekende
samenstelling van de vloeistoffase is vergeleken met speciatie data (met een NMR
Samenvatting xv
techniek) uit de literatuur. De berekende speciatie met het E-EOS model bleek goed
overeen te komen met de NMR data. In Appendix A zijn nieuwe CO2
oplosbaarheidsdata gepresenteerd bij verschillende beladingen (0.047 – 1.105
mol.mol-1
), temperatuur (283 en 298 K), MDEA concentratie (35 en 50 wt.%) en
methaan partiaal druk (tot 69 bar). Uit deze experimenten en E-EOS simulaties
bleek dat de totaal druk en/of methaan partiaal druk een groot effect heeft op de
oplosbaarheid van CO2 in waterig MDEA. Het is gebleken dat de oplosbaarheid van
CO2 afneemt met toenemende methaan partiaal druk. Uit de simulaties met het E-
EOS model bleek dat deze afnemende oplosbaarheid wordt veroorzaakt doordat de
CO2 fugaciteits coëfficient lager wordt met toenemende methaan partiaal druk.
De in hoofdstuk 3 beschreven “electrolyte equation of state” is verder ontwikkeld in
hoofdstuk 4 om de oplosbaarheid van H2S in een waterige MDEA oplossing te
kunnen berekenen. Verschillende (H2S specifieke) pure component en binaire
interactie parameters zijn toegevoegd aan het E-EOS model. Dit model is
vervolgens gevalideerd met oplosbaarheidsdata van H2S in een waterige MDEA
oplossing met en zonder de aanwezigheid van methaan als make-up gas. In
appendix A zijn nieuwe H2S oplosbaarheids data gepresenteerd in een waterige
MDEA oplossing bij verschillende beladingen (0.028 – 0.075 mol.mol-1
),
temperatuur (283 en 298 K), MDEA concentratie (35 en 50 wt.%) en methaan
partiaal druk (tot 69 bar). Voor beide systemen (H2S-MDEA-H2O en H2S-MDEA-
H2O-CH4) berekent het model een te lage H2S partiaal druk (d.w.z. een te hoge
oplosbaarheid). Echter, de voorspellingen van het model, wanneer geen methaan
aanwezig is, zijn beter. Zowel uit de resultaten van de model berekeningen als uit
de experimenten bleek dat de oplosbaarheid van H2S afneemt bij een toenemende
methaan partiaal druk. Uit de berekeningen met het E-EOS model bleek dat de
afnemende oplosbaarheid werd veroorzaakt doordat de fugaciteitscoefficient van
H2S afneemt met toenemende methaan partiaal druk.
In hoofdstuk 5 is de oplosbaarheid van CO2 en H2S in waterig MDEA bestudeerd,
wanneer deze gassen gelijktijdig aanwezig zijn en methaan wel en niet aanwezig is
xvi Samenvatting
als inerte component. Er zijn 72 nieuwe oplosbaarheidsdata gepresenteerd voor 35
en 50 wt.% MDEA bij 283 en 298 K en bij verschillende beladingen. De methaan
partiaal druk is gevarieerd van 6.9 tot 69 bar. Het blijkt dat de H2S partiaal druk
aanzienlijk toeneemt met toenemende CO2 belading, d.w.z. de capaciteit voor H2S
afvang neemt af. De experimentele resultaten zijn vergeleken met het “electrolyte
equation of state” model voor enkelvoudige gassen, zoals dit beschreven is in
hoofdstuk 3 en 4 van dit proefschrift. Wanneer zowel CO2 als H2S tegelijk aanwezig
zijn, is slechts één nieuwe parameter nodig. Dit is de CO2-H2S moleculaire
interactie parameter. Tijdens de simulaties met het E-EOS model bleek dat de
model resultaten niet gevoelig waren voor deze parameter. Het E-EOS model is in
eerste instantie gebruikt om de model resultaten te vergelijken met oplosbaarheids
data uit de literatuur voor het systeem CO2-H2S-MDEA-H2O. In het algemeen mag
geconcludeeerd worden dat het E-EOS model de oplosbaarheid van CO2 en H2S
gelijktijdig aanwezig in waterig MDEA goed kan beschrijven. Het E-EOS model is
ook vergeleken met de experimentele data van het CO2-H2S-MDEA-H2O-CH4
systeem, zoals gepresenteerd in hoofdstuk 5. Het model kan deze experimentele
gegevens ook goed beschrijven.
Gebaseerd op de resultaten in dit proefschrift, kan geconcludeerd worden dat de
“electrolyte equation of state” (E-EOS) aanpak veelbelovende resultaten oplevert
om de thermodynamica van zuur gas – alkanolamine systemen te beschrijven. Het
is aangetoond dat het model kan worden uitgebreid van binaire niet-reactieve
systemen, tot reactive enkelvoudige gas systemen (CO2 of H2S) en tot reactive
systemen waarin deze zure gassen gelijktijdig aanwezig zijn. Naar verwachting kan
het model nog aanzienlijk verbeterd worden, wanneer meer fysische en chemische
evenwichts data beschikbaar zijn.
Onderstaande data zijn bijvoorbeeld zeldzaam in de (“gas treating”) literatuur:
• Binaire thermodynamische data
Vloeistof damp evenwichten, meng enthalpy, etc. van binaire water
alkanolamine systemen;
Samenvatting xvii
• Speciatie data van reactive zuur gas – alkanolamine systemen
Op dit moment worden de verschillende ionische interactie parameters
bepaald met behulp de totale oplosbaarheid van zuur gas in het
oplosmiddel. Echter deze parameters kunnen veel nauwkeuriger bepaald
worden, wanneer de concentratie van de verschillende moleculaire en
ionische componenten in de vloeistoffase bekend is. Ook de concentratie
van het moleculaire CO2 in de vloeistoffase kan dan rechtstreeks bepaald
worden en hoeft niet meer afgeschat te worden met behulp van de CO2-
N2O analogie, zoals gedaan is in dit proefschrift;
• Thermodynamische data bij hoge (methaan) partiaal drukken
In het algemeen worden de thermodynamische data bepaald bij lage
(atmosferische) druk. In dit proefschrift echter is bewezen dat de (methaan
partiaal) druk een grote invloed heeft op de totale oplosbaarheid van zuur
gas. Er is meer onderzoek nodig om de invloed van inerte componenten
(zoals stikstof, zuurstof of andere koolwaterstoffen) op de oplosbaarheid
van zure gasen in waterige alkanolamine oplossingen goed te kunnen
beschrijven.
xviii Samenvatting
xix
Contents
SUMMARY vii
SAMENVATTING xiii
1 GAS TREATING PROCESSES 1
1.1 TREATING METHODS 1
1.2 AMINE TREATING PLANT 4
1.3 GAS TREATING FUNDAMENTALS 6
1.4 THIS THESIS 9
REFERENCES 11
2 MODELS OF ACID GAS SOLUBILITY IN ALKANOLAMINE
SOLUTIONS 13
2.1 THERMODYNAMIC INTRODUCTION 14
2.1.1 Classical thermodynamics 14
2.1.2 Activity and fugacity 16
xx Contents
2.2 SIMPLE MODELS NEGLECTING ACTIVITY
COEFFICIENTS 17
2.2.1 Kent-Eisenberg (1976) 18
2.2.2 Posey et al. (1996) 19
2.3 MODELS USING THE GAMMA –PHI METHOD 20
2.4 EQUATIONS OF STATE 24
2.5 ELECTROLYTE SOLUTIONS 26
2.5.1 Debye-Hückel Approach 26
2.5.2 Mean Spherical Approximation Approach 29
2.6 DISCUSSION OF THE MODELS 32
2.6.1 Semi-empirical models versus rigorous
models 32
2.6.2 Excess Gibbs energy models versus
electrolyte equations of state 33
2.7 CONCLUSION 36
LIST OF SYMBOLS 37
REFERENCES 39
3 SOLUBILITY OF CARBON DIOXIDE IN AQUEOUS
N-METHYLDIETHANOLAMINE 43
3.1 INTRODUCTION 44
3.2 THE ELECTROLYTE EQUATION OF STATE 46
3.2.1 General 46
3.2.2 The pure component model 47
3.2.3 Mixing rules 48
3.2.4 Electrolyte interactions 51
3.2.5 Chemical reactions 53
Contents xxi
3.3 MODEL DEVELOPMENT 54
3.3.1 Former work 54
3.3.2 Chemical reactions 55
3.3.3 Binary molecular interaction parameters 56
3.3.4 Binary ionic interaction parameters 66
3.4 MODELING RESULTS 69
3.4.1 Ternary system CO2-MDEA-H2O 69
3.4.2 Quaternary system CO2-MDEA-H2O-CH4 76
3.5 CONCLUSIONS 79
LIST OF SYMBOLS 80
REFERENCES 82
4 SOLUBILITY OF HYDROGEN SULFIDE IN AQUEOUS
N-METHYLDIETHANOLAMINE 87
4.1 INTRODUCTION 88
4.2 THE ELECTROLYTE EQUATION OF STATE 89
4.3 MODEL DEVELOPMENT 90
4.3.1 Former work 90
4.3.2 Chemical reactions 91
4.3.3 Pure component model 92
4.3.4 Binary molecular interaction parameters 93
4.3.5 Binary ionic interaction parameters 101
4.4 MODELING RESULTS 108
4.4.1 Ternary system H2S-MDEA-H2O 108
4.4.2 Quaternary system H2S-MDEA-H2O-CH4 119
4.5 CONCLUSIONS 123
LIST OF SYMBOLS 124
REFERENCES 126
xxii Contents
5 SOLUBILITY OF CARBON DIOXIDE AND HYDROGEN
SULPHIDE IN AQUEOUS N-METHYLDIETHANOLAMINE 131
5.1 INTRODUCTION 132
5.2 THE ELECTROLYTE EQUATION OF STATE 133
5.3 EXPERIMENTAL 134
5.3.1 Experimental setup and procedure 134
5.3.2 Experimental results 135
5.3.3 Discussion 140
5.4 MODEL RESULTS 143
5.4.1 System CO2-H2S-MDEA-H2O 143
5.4.2 System CO2-H2S-MDEA-H2O-CH4 147
5.5 CONCLUSIONS 152
LIST OF SYMBOLS 153
REFERENCES 154
APPENDIX A SOLUBILITY OF H2S AND CO2 IN AQUEOUS
SOLUTIONS OF N-METHYLDIETHANOLAMINE 155
A.1 INTRODUCTION 156
A.2 EXPERIMENTAL 157
A.3 RESULTS 159
A.3.1 Experiments with CO2 159
A.3.2 Experiments with H2S 162
A.3.3 Discussion 164
Contents xxiii
A.4 VALIDATION OF THE MODEL 165
A.4.1 Model description 165
A.4.2 Validation of the Solbraa model 167
A.4.3 Influence of experimental database 169
A.4.4 Influence of the MDEA dissociation
constant (Ka) 172
A.4.5 Influence of the binary interaction
parameters 174
A.5 CONCLUSIONS AND RECOMMENDATIONS 178
LIST OF SYMBOLS 180
REFERENCES 181
LIST OF PUBLICATIONS 185
CURRICULUM VITAE 187
DANKWOORD 189
xxiv Contents
1
Chapter 1
Gas Treating Processes
1.1 Treating methods
Acid gases such as carbon dioxide (CO2), hydrogen sulphide (H2S), carbonyl
sulphide (COS) and mercaptans (RSH), are often present in industrial gas streams.
They have to be removed in large amounts for several reasons:
• To reduce corrosion
The presence of acid components and water may result in severe corrosion
of process equipment;
• To improve plant operation and economy
When these gases are present in large amounts, they lower the heating
value of the gas or decrease plant or pipeline capacity;
• For safety and the environment
H2S, COS and RSH are toxic components and even small amounts may
cause severe health problems. CO2 is an important greenhouse gas and
capture and storage of huge amounts of it are required to stop the global
warming problem.
2 Chapter 1
The process conditions for these gas treating (or sweetening) processes vary
widely. For example flue gas from a coal fired power plant contains 12–15 % CO2 at
atmospheric pressure, while the main component is nitrogen. However, a typical
natural gas stream has a high pressures and mainly contains CH4, while acid
components such as CO2, H2S, COS and RSH may be present up to 30 % of the
whole.
Which kind of gas treating process is used depends on the specifications of the
treated gas. These specifications can be determined by environmental regulations
(total sulphur specification), the heating value of the gas (CO2 concentration) or
downstream process limitations. Typical specifications of the treated gas for the
various applications are given in Table 1.
CO2 H2S
Natural gas 2-3 % (v/v) < 4 ppm
LNG < 50 ppm < 4 ppm
Syngas (Oxo) 10-100 ppmv < 1ppm
Syngas (ammonia) < 500 ppmv -
Refinery streams no specifications 4 – 150 ppm
Tail gas None < 250 ppm
Flue gas 85-95 % removal -
Table 1 Typical gas specifications [1]
The processes which are currently available for the removal of acid gases vary
widely. Single wash operations can be used, but also complex multi-step recycle
units may be required to meet the requirements. Below an overview of the different
gas purification processes is given [2]:
• Chemical absorption
The most important process for the removal of acid gases is the chemical
absorption in an aqueous alkanolamine solution. In this process the acid
gas is contacted with the solvent in an absorber. A reversible reaction takes
Gas treating processes 3
place and the solvent is regenerated in a stripper at an elevated
temperature or lower pressure. The advantage of this process is the low
partial pressure of the acid gas, that can be obtained in the absorber outlet.
The main disadvantage is the high energy costs of regeneration. When the
total sulphur content is very low and gas outlet concentrations are stringent,
a scavenger can be considered as absorption liquid for the removal of
sulphur components. The reaction between acid gas and a scavenger is
irreversible, so regeneration is not possible. The loaded scavenger can be
treated as waste or discharged to sea after treatment;
• Physical absorption
Acid gas absorption in physical solvents (glycols or ethers) is normally used
for bulk separation of carbon dioxide and/or hydrogen sulphide, when the
acid gas is available at high partial pressure and deep removal is not
required. Because no chemical reaction takes place between acid gas and
the solvent, regeneration costs are low compared to those of chemical
absorption. When the acid gas is available at a partial pressure higher than
15 bar, physical absorption is usually attractive. For acid gas partial
pressures lower than 5 bar, chemical absorption tends to be more
favourable;
• Adsorption
Adsorption is the process of binding vapor molecules in the pores of a
microporous solid. The acid components are concentrated on the solid
surface by forces existing at this surface. Forces between the acid gas and
adsorbent can be both physical and chemical. Commercial adsorbents
mostly use physical adsorption, because they can be regenerated more
easily. Molecular sieves based on zeolite structures, are commonly used as
adsorbent in gas treating, because they have a high adsorption selectivity
for polar components such as H2O, CO2, H2S, COS and RSH. In this way
these components can be easily removed from the non-polar components
such as CH4 or H2. Adsorption can be a suitable process, where H2S has to
be removed, the total amount of sulphur is very small, and also other
4 Chapter 1
sulphur components (such as mercaptans (RSH)) have to be removed.
Normally, two parallel units are installed, where one unit is in the adsorbing
mode and the other in the regeneration mode;
• Membranes
Membrane technology is a new development in the gas treating industry. In
a membrane separation process the components are separated by a
difference in diffusion rates through a thin polymer barrier. The diffusion
rate through the membrane is determined by the component and
membrane characteristics and the partial pressure difference of the specific
component across the membrane. Membranes are mostly used for bulk
separation. However, when multiple stages, recycle streams or a
combination with other technologies are used, also high purities are
possible. The main disadvantage of membrane units is their tendency to
become plugged, so normally a clean feed is required.
The processes described above are the most important unit operations used in gas
treating. To combine the advantages also combinations of these processes are
used. For example a hybrid solvent, which contains both a physical as a chemical
absorbent, can be used for treating of gas streams where acid partial pressures are
intermediate. The bulk separation is carried out by the physical absorbent while the
deep removal is carried out by the chemical solvent.
1.2 Amine treating plant
One of the most common processes in the gas industry is absorption / desorption
with an aqueous alkanolamine solution. Alkanolamines are chemicals which contain
at least one nitrogen group and one alcohol group. The nitrogen group is
responsible for the required alkalinity of the molecule and the alcohol group reduces
the vapor pressure, and thus losses in the regenerator are minimised.
Alkanolamines are classified by the number of non-hydrogen atoms attached to the
Gas treating processes 5
nitrogen atom in primary, secondary and tertiary amines. In this work MDEA (N-
methyldiethanolamine; a tertiary amine) is studied, because this is one of the most
commonly used alkanolamines in the gas treating industry. The reaction between
CO2 and aqueous MDEA is relatively slow, compared to the reaction with H2S.
Therefore, this amine is commonly used in processes where H2S has to be
removed selectively from a gas stream containing both CO2 and H2S.
In Figure 1 the basic process flow diagram of a typical amine treating plant is
shown.
REBOILER
LEAN SOLVENT COOLER
REGENERATOR
ACID GAS COOLER
REFLUX DRUM
Make Up Water
ABSORBER
Condensate
Steam
Rich solvent
acid gas
Feed Gas
Treated Gas
Flash Gas
FLASH DRUM
Lean solvent
Optional
Figure 1 Basic process flow diagram of a gas treating plant
The acid gas stream, enters the absorber at the bottom and is contacted counter-
currently with the aqueous alkanolamine solution. The absorber, which can be filled
with trays or packing material typically has an operating temperature between 20
and 40 °C. The lower the operating temperature, the higher the acid gas solubility.
However, the reaction rate between acid gas and amine decreases with decreasing
temperature. For high pressure natural gas treatment, an intermediate flash step
can be used to release dissolved hydrocarbons, which are co-absorbed in the
absorber. The rich amine solution is flashed and heated in a heat exchanger by lean
6 Chapter 1
solvent from the bottom of the regenerator. The heated rich solvent enters the
regenerator at the top of the column. In the regenerator the acid gases are released
from the liquid with steam as stripping agent. The lean solution in the stripper is
cooled in the heat exchanger with cold rich amine and further cooled before it is
sent back to the top of the absorber. The gas that is released in the regenerator is
cooled to condense the water. The condensed water is sent back to the stripper; the
concentrated acid gas stream can be sent to a Claus unit for sulphur removal or can
be prepared for disposal.
1.3 Gas treating fundamentals
For the reliable design of equipment in gas treating plants the following information
has to be available:
• Physical, thermal and transport parameters; such as. kG, kL and a. Empirical
correlations are available in the literature for these parameters;
• Reaction kinetics;
• Vapor-liquid equilibrium data (VLE).
In Figure 2 the parameters (according the film model) for the driving force in a
countercurrent gas-liquid system without chemical reaction are shown:
Gas treating processes 7
LIQUID
GAS
G
G
G
Dk
δ=
solubility
mass transfer
mass transfer
&
kinetics
driving force
m=CL,i
/CG,i
Gδ
Lδ
L
L
L
Dk
δ=
CG
CG,i
CL,i
CL
Figure 2 Driving force for a gas – liquid process according to the film model
Gas and liquid resistances are determined by the diffusion coefficients and the film
thickness in both phases. In the film model it is assumed that equilibrium exists at
the gas-liquid interface. For an acid gas-alkanolamine system, where a chemical
reaction takes place in the liquid, mass transfer in the liquid may be enhanced by
the chemical reaction. In this thesis the acid gas solubility in the aqueous
alkanolamine solution (VLE) is discussed. The acid gas solubility is defined as the
relation between the partial pressure acid gas (or more precisely the fugacity) and
the concentration of acid gas in the liquid at equilibrium conditions for a specified
temperature, pressure and amine liquid concentration. Many experimental VLE data
have been reported in the literature at different process conditions. In Figure 3 some
VLE data measured by different researchers are presented for the CO2 solubility in
20 wt. % aqueous DEA.
8 Chapter 1
0.001
0.01
0.1
1
10
100
0.01 0.1 1
Liquid loading [moleCO2/mole amine]
PC
O2 [k
Pa
]
.
Haji-Sulaiman (1998)
Bullin (1997)
Haji-Sulaiman (1996)
Bullin (1997)
Lee (1974)
this work
Figure 3 Solubility of CO2 in 20 wt.% DEA at 323 K
The scatter in the reported experimental data is large, especially in the low loading
regime. All these experimental data can be used for preliminary calculations, but
thermodynamic models are required to develop a consistent VLE dataset, to
interpolate and extrapolate the data to the required process conditions, and to
predict VLE in flowsheet simulation programs.
The driving force for mass transfer as calculated in flowsheet simulators, is usually
based on the difference in concentrations between the different phases. However, it
has been shown that this approach results in inconsistencies and a more consistent
approach is required to predict mass transfer. For example Haubrock [3] has shown
that, when the kinetic relation is based on concentrations, the reaction between OH-
and CO2 is influenced significantly by the counter-ion, which does not take part of
the chemical reaction. However when activities of each species are used (instead of
concentrations) a unique activity independent kinetic correlation can be derived.
Gas treating processes 9
Therefore rigorous thermodynamic models are required in process simulators and
the reaction rates should be based on activities instead of concentrations to make
the process design more consistent.
1.4 This thesis
In this thesis the solubility of the acid gases CO2 and H2S in aqueous N-
methyldiethanolamine is studied experimentally and theoretically. Also the influence
of methane (the main component in natural gas) on the acid gas solubility is
investigated quantitatively. Experimental solubility data of this system have been
determined in a stirred cell and these data were compared with an electrolyte
equation of state (E-EOS). This equation is used for both the vapor and the liquid.
Below a short outline of the structure of this thesis is presented.
In Chapter 2 a review of the several thermodynamic models, which can be used to
predict the acid gas solubilities is presented and discussed. The content of this
chapter has been presented during:
• 56th Laurance Reid Gas Conditioning Conference (2006) Norman,
Oklahoma.
In Chapter 3 the solubility of CO2 in aqueous MDEA is discussed quantitatively. An
electrolyte equation of state is developed to predict the solubility of CO2 in aqueous
MDEA. This thermodynamic model has been compared with experimental solubility
data from open literature. Also a comparison with the experimental data (CO2-
MDEA-H2O-CH4) as presented in appendix A has been carried out. The content of
this chapter has been published in:
• P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F. Versteeg, Fluid Phase
Equilibria 264 (2008) 99-112.
10 Chapter 1
In Chapter 4 the solubility of H2S in aqueous MDEA is studied. The E-EOS
developed in Chapter 3 is further developed to describe the solubility of H2S in
aqueous MDEA in the presence of methane. The model is compared with H2S
solubility data from open literature (H2S-MDEA-H2O) and from Appendix A of this
thesis (for H2S-MDEA-H2O-CH4). The content of this chapter has been published in:
• P.J.G. Huttenhuis, N.J. Agrawal, G.F. Versteeg, International Journal of Oil,
Gas and Coal Technology 1 (2008) 399-424.
In Chapter 5 the simultaneous absorption of CO2 and H2S in aqueous MDEA is
studied. New experimental solubility data of CO2 and H2S in aqueous MDEA are
presented at methane pressures up to 69 bar. These experimental data are
compared with the E-EOS developed in Chapters 3 and 4. Only one new binary
interaction parameter is required to describe the quarternary system CO2-H2S-
MDEA-H2O from the ternary systems discussed in Chapters 3 and 4. The content of
this chapter has been published in:
• P.J.G. Huttenhuis, N.J. Agrawal, G.F. Versteeg, Industrial & Engineering
Chemistry Research 48 (2009) 4051-4059.
In Appendix A several experimental CO2 and H2S solubility data are presented. The
influence of the methane partial pressure (up to 69 bar) on the solubility of CO2 and
H2S (single gas) in aqueous MDEA is presented. The content of this chapter has
been published as:
• P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Journal
of Petroleum Science and Engineering 55 (2007) 122–134.
Gas treating processes 11
References
[1] R. Wagner, B. Judd., Fundamentals – Gas Sweetening, Laurance Reid Gas
Conditioning Conference, Norman, Oklahoma (2006).
[2] A.L. Kohl, R.B. Nielsen, Gas Purification 5th Ed., Gulf Publishing Company,
Houston (1997).
[3] J. Haubrock, The process of dimethylcarbonate to diphenyl carbonate:
thermodynamics, reaction kinetics and conceptual process design, Ph.D.
thesis, Twente University (2007).
12 Chapter 1
13
Chapter 2
Models of Acid Gas Solubility in
Alkanolamine Solutions
Abstract
This chapter considers models to predict the solubility of acid gasses in
alkanolamine solutions. Acid gases such as CO2 and H2S are commonly removed
with alkanolamine solutions in natural gas treating plants, refineries and LNG plants.
Also in power plants alkanolamines will probably be used more frequently, because
requirements for CO2 exhaust in flue gases will become stricter in the near future.
For the design of gas treating equipment, one of the most important parameters is
the acid gas solubility in the liquid. This solubility needs to be known at the different
conditions in the plant. Because many different conditions are encountered,
collection of all data by experiments is impossible. This is complicated by the fact
that data of different authors show a lot of scatter. For these reasons reliable
thermodynamic models are necessary, which can predict the acid gas solubility
accurately. In this chapter an overview of such thermodynamic models will be
presented.
14 Chapter 2
dU TdS PdV= −
dQdS
T≥
dU dQ dW= −
Thermodynamic models are usually grouped as follows:
• (Semi)-empirical models: These models are based on mass balances,
reaction equations and physical solubility constants. One of the equilibrium
constants is used as a fit parameter;
• Excess Gibbs energy models: In these models the gas phase is modelled
with an equation of state and the liquid phase properties are calculated with
an excess Gibbs energy model;
• Electrolyte equation of state: In these models both gas and liquid phase are
modelled with an equation of state with several ionic terms added to the
equations.
2.1 Thermodynamic introduction
2.1.1 Classical thermodynamics
As mentioned this chapter considers thermodynamic models which are capable of
predicting the VLE of acid gas – alkanolamine solutions. To explain the origin of
these models, some thermodynamic considerations will first be presented. Most
thermodynamic relations are derived from the first law (conservation of energy) and
second laws (entropy production) of thermodynamics:
Equation 1
Equation 2
From these equations the following relation between the internal energy, the
intensive properties T and P, and the extensive properties S and V can be obtained:
Equation 3
Thermodynamic models 15
0i i
i
SdT VdP n d μ− + =�
( , , )i i
i
G U PV TS dG T P n SdT VdP nμ= + − = − + +�
This equation is only applicable for a closed thermodynamic system. To describe an
open system, where material is exchanged with the surroundings, an additional
term is needed:
Equation 4
�i is called the chemical potential of a component and is a function of pressure,
temperature and composition. The internal energy U is a first order homogeneous
function in the extensive variables S, V and n. Euler’s theorem of homogeneous
functions tells that with this equation for the internal energy U each thermodynamic
system can be described as:
Equation 5
When this equation is differentiated and compared with Equation 4, the Gibbs-
Duhem equation follows:
Equation 6
This is the fundamental thermodynamic equation for an open system. The internal
energy can be calculated as function of the independent variables S, V and n.
However, normally it is more convenient to use other independent variables,
because entropy is difficult to quantify. These additional relations contain the same
information as the fundamental equation above. However, they depend on variables
such as pressure (P) and temperature (T), that are easier to measure. For this
reason the Gibbs energy (G) and Helmholtz (A) energy have been introduced:
Equation 7
Equation 8
, ,j
i i i
i ii S V n
UdU TdS PdV dn TdS PdV dn
nμ
� �∂= − + = − +� �
∂� �� �
, ,
, ,
( , , )
j
V n S n
i S V n i i
i ii
U UU U S V n S V
S V
Un TS PV n
nμ
∂ ∂� � � �= = + +� � � �
∂ ∂� � � �
� �∂= − +� �
∂� �� �
( , , )i i
i
A U TS dA T V n SdT PdV nμ= − = − − +�
16 Chapter 2
, , , , , ,j j j
i
i i iS V n T P n T V n
U G A
n n nμ
� � � � � �∂ ∂ ∂= = =� � � � � �
∂ ∂ ∂� � � � � �
0
0ln
i i
PRT
Pμ μ− =
From the definition of the chemical potential (�i) it follows that:
Equation 9
Equilibrium thermodynamics needs to describe the distribution of each component
in the different phases quantitatively. At equilibrium conditions the Gibbs energy has
a global minimum and the temperature (T), pressure (P) and chemical potential (�i)
of each component is uniform in the whole system. So the following relation is
applicable to a gas – liquid system:
2.1.2 Activity and fugacity
The chemical potential of a component is a rather abstract property depending on
temperature, pressure and composition. Because an absolute value of the chemical
potential is not defined an arbitrary reference state has to be chosen. From the
Gibbs-Duhem relation (Equation 6) and the ideal gas law the chemical potential of a
pure, ideal gas at isothermal conditions can be derived from the chemical potential
�i0 of that gas at the standard pressure P
0:
Equation 10
It is not inconvenient to use the chemical potential in equilibrium calculations and
therefore the fugacity is introduced:
Equation 11
Equation 11 is applicable to gases, liquids and solids. For a pure, ideal gas the
fugacity is equal to the pressure P for a component i in an ideal gas it is equal to the
partial pressure yiP. This relation between the chemical potential and the fugacity
0
0ln i
i i
i
fRT
fμ μ− =
v l
i iμ μ=
Thermodynamic models 17
can be used to translate abstract thermodynamic variables into physical variables. It
is difficult to quantify the chemical potential, but the fugacity can be considered as a
pseudo-pressure. The ratio of 0
i
i
f
fis called the activity ai of component i. This
activity of a component indicates how “active” the component is compared to its
standard state.
Equation 9 and Equation 11 combine to give fugacity coefficients (i
i
i
f
Pϕ = ) which
can be calculated from the residual Gibbs Gr or Helmholz A
r energy:
Equation 12
The residual Gibbs energy and Helmholz energy are the difference in the actual
energy and the energy assuming ideal gas conditions. This method for the gas is
general and can be applied to liquids as well.
2.2 Simple models neglecting activity coefficients
The first VLE models for weak electrolyte solutions, such as acid gas – aqueous
alkanolamine systems, did not incorporate activities. Van Krevelen et al. [27] used
“apparent” equilibrium constants in their VLE model. In their equations for chemical
equilibrium they used concentrations instead of activities and these “apparent”
equilibrium constants were fitted with experimental data with a function of ionic
strength. Danckwerts et al [5] used the same approach for predicting VLE data for
the solubility of CO2 in an aqueous amine solution.
, ,
, ,
ln ( , , )
( , , ) ln
j
j
r
i
i T P n
r
i T V n
RT G T P nn
A T V n RT Zn
ϕ� �∂
= =� �∂� �
� �∂−� �
∂� �
18 Chapter 2
2 23 3
2
[ ' ] [ ] [ ' ] [ ] CO
t e e e
CO
PRR NH HCO RR NCOO CO
Hα
− − −= + + +
2
2 3 3[ ' ] [ ] [ ' ] 2[ ]e e e e
RR NH HCO RR NCOO CO+ − − −
= + +
2 2 2[ ]CO CO
P H CO=
2[ ' ] [ ' ] [ ' ] [ ' ]t e e e
RR NH RR NH RR NH RN NCOO+ −
= + +
2.2.1 Kent-Eisenberg (1976)
Kent and Eisenberg [15] adapted the Danckwerts approach to the solubility of H2S
and CO2 in aqueous solutions of MEA and DEA. Later researchers also used this
model for other amine-acid gas systems. In this VLE model a set of non-linear
equations has to be solved simultaneously. Non-idealities that are present in the
system are not incorporated in the activities, but these non-idealities are lumped
together in one or more of the chemical equilibrium constants. The involved
chemical reactions are used in the model. In addition to these reaction equilibrium
equations, the following set of component balances must be solved simultaneously:
Amine balance:
Equation 13
CO2 balance:
Equation 14
Moreover, to assure electro neutrality of the solvent the electron balance has to be
taken into account:
Electron balance:
Equation 15
The parameter � is the acid gas liquid loading. The concentration of molecular CO2
in the liquid phase is estimated with Henry’s law:
Equation 16
For the chemical equilibrium constants data published in literature are used, except
for the amine protonation and carbamate formation reactions. These two
Thermodynamic models 19
parameters are used as adjustable parameters. While using these equilibrium
constants as fit parameters, the calculated acid gas partial pressure is forced to
match the available experimental VLE data for single gas – single amine
experiments. The resulting apparent equilibrium constants are used to carry out the
VLE calculations. It appears that good VLE predictions can be obtained in the
loading range of 0.2-0.7 mole acid gas / mole amine. For higher and lower loadings
the model is not successful. The model is also not successful for tertiary amines,
because these do not form carbamates and one adjustable parameter less is
available for parameter fitting (Solbraa [26]).
2.2.2 Posey et al. (1996)
Another simple model was developed by Posey et al. [21], using only one chemical
reaction for the CO2-amine system and one reaction for the H2S-amine system. In
this model the equilibrium partial pressure of the acid gas component is calculated
with a single semi-empirical formula, instead of solving a set of equations. The
following chemical reaction equations are used in this model:
Equation 17
Equation 18
Formation of S2-
, CO32-
and OH- ions is neglected in this model. Introducing an
apparent equilibrium constant, a total acid gas liquid loading factor � and Henry’s
law, the following semi-empirical equation for CO2 can be derived:
Equation 19
Here KCO2 is a product of the apparent equilibrium constant of Equation 17 and
Henry constant and XCO2 is the mole fraction of bicarbonate (HCO3-) in the liquid. In
this model it is assumed that all absorbed CO2 reacts to bicarbonate. The
equilibrium constant KCO2 is assumed to be a function of temperature T, amine mole
2 2 3[ ] [ ] [ ] [ ] [ ]Am CO H O AmH HCO+ −
+ + ←⎯→ +
2[ ] [ ] [ ] [ ]Am H S AmH HS+ −
+ ←⎯→ +
2 2 2(1 )
CO CO COP K x
α
α=
−
20 Chapter 2
fraction X
oamine and total acid gas liquid loading � according the equation presented
below:
Equation 20
The unknown model parameters (A, B, C, and D) of the model are determined by
regressing the model with experimental data points from literature. For each
experimental point the equilibrium constant KCO2 is calculated using Equation 20.
The natural logarithm of this equilibrium constant is fitted by linear regression using
Equation 20. For the H2S-amine system the same equations as described above
can be used.
The four model parameters have been determined for the following acid gas –
amine pairs: MDEA-CO2, MDEA-H2S and DEA-H2S. Model predictions for MDEA-
CO2 and MDEA-H2S have an accuracy of 20 and 22 % respectively, while the
absolute deviation for DEA-H2S is 60%. It should be remembered that acid gas
partial pressures vary over seven orders in magnitude. It appears that Posey’s
model can be used for checking the consistency of different experimental data sets
and providing an initial guess value for rigorous VLE calculations. However, with
this model it is not possible to calculate the speciation of the different molecules and
ions present in the liquid. For this reason the model cannot be used in rate based
gas treating simulators, because for these calculations, actual concentrations of
each species should be known at each location in the column.
2.3 Models using the Gamma – Phi method
Most of the rigorous VLE models used in the gas treating industry are based on the
so called gamma-phi (�-�) method. Other names for these models are activity
models or excess Gibbs energy models. In these models the activity of the liquid
phase � is calculated separately and in a way different from that of the fugacity of
the vapor phase �. The activity of the liquid is calculated with an excess function,
while the fugacity of the vapor is calculated with an equation of state. An excess
0.5
2 min minln ( )o o
CO a e a e
BK A C X D X
Tα α= + + +
Thermodynamic models 21
2 2
1 2 1 2 2 1ln lnEg Ax x RT Ax RT Axγ γ= = =
function is defined as the difference between the values of actual properties of a
mixture and their values calculated for an ideal mixture at the same conditions; i.e.
composition, temperature and pressure, if an excess Gibbs energy equation is used
(see Equation 7). The excess thermodynamic properties (entropy, volume and
chemical potential) of a component i are determined by differentiation of the molar
excess Gibbs energy.
Calculations in the liquid
To describe the thermodynamic properties of the liquid, the excess Gibbs energy GE
has to be known as function of temperature, pressure and liquid composition. These
equations can be determined from theoretical considerations or from experimental
data for binary, ternary and multi-component mixtures. However, reduction of
information is required, because such a detailed description becomes far too
complicated. Most commonly the thermodynamic system is represented by using
pure component and binary interaction data only. These pure component and binary
interaction data can be obtained from experimental VLE data. Many expressions
relating GE to the composition and activities have been proposed in literature. The
theoretical background of these equations is weak. The most equations contain one
or more adjustable parameters that are dependent on temperature. The older
empirical models of Margules [18] and van Laar [28] are mathematically easier to
handle than the newer models of Wilson [29], Renon and Prausnitz (NRTL model,
[23]), Abrahams and Prausnitz (UNIQUAC, [1]), However, predictions with these old
models are good for many moderately nonideal binary mixtures. The simplest model
is the one-parameter Margules model [18]. The relation for the excess Gibbs
Energy in this model is given below:
Equation 21
A is an empirical interaction parameter which is determined from experimental data.
For strongly nonideal binary mixtures, such as alcohols with hydrocarbons, so-
called local composition models are required. The idea is that the liquid is
composed of hypothetical fluids, each consisting of a central molecule surrounded
22 Chapter 2
by other molecules. Because the interactions differ for each orientation of the
molecules, different local compositions exist. The thermodynamic properties for the
real solutions are calculated from the properties of the hypothetical mixture. A
commonly used local composition model it that of Wilson [29]. In this model only two
adjustable interaction parameters are required which are related to the energy of
interaction between the governing molecules. This model can be used for highly
non-ideal binary systems. However, it cannot handle immiscible liquid phases.
Renon and Prausnitz [23] developed the NRTL model, by introducing an additional
“non-randomness” parameter. Usually, this parameter has a value between 0.20
and 0.47 (Prausnitz et al, ref.[22]). However, when the liquid mixture is completely
random this parameter should be zero. The interaction parameters can be
considered temperature independent in a narrow temperature range. For wider
ranges a linear temperature dependency is suggested. Drawback of this
temperature dependency is that the number of fit parameters is doubled. The major
disadvantage of the NRTL is that three interaction parameters are required to
describe each binary system. When experimental data are lacking this introduces a
problem.
To avoid this, Abrahams and Prausnitz [1] developed the UNIQUAC model. In this
thermodynamic model a distinction is made between a combinatorial part, requiring
only pure component data and a residual part depending on intermolecular forces.
The main advantage of this model is that it is relatively simple, containing only two
adjustable interaction parameters, while a lot of non-ideal binary systems, including
partly immiscible liquids, can be described satisfactorily.
Another commonly used approach to calculate the activity coefficient of a mixture, is
the group-contribution method. In this approach a molecule is separated in different
functional groups and the total molecule-molecule interactions are the weighted
sums of the different group contributions. When group contributions are determined
from suitable experiments, activity calculations can be carried out with other
molecules without the need for additional experiments. This is attractive when
Thermodynamic models 23
calculations have to be carried out, as difficult and expensive experiments may not
be necessary. The most commonly used group contribution model is UNIFAC
(UNIversal Functional Activity Coefficient) originally proposed by Fredenslund et al.
[7].
As already discussed, binary activity models can easily be extended to multi-
component systems, without introducing additional assumptions or parameters. In
this chapter it is not the aim to provide all GE equation for the different activity
models; only the main relations are presented:
Equation 22
From Equation 22 it can be seen, that the activity coefficient can be calculated,
when the excess Gibbs energy relation is known:
Equation 23
Calculations in the vapor
In the excess Gibbs energy models properties of the vapor are calculated in a way,
different from than described above for the liquid. The fugacity coefficient of the
vapor is calculated by differentiating the Gibbs energy. This yields the following
equation:
Equation 24
This equation can be used, when the P-V-T relation is described by an equation
with P and T as the independent variables; i.e. the relation is explicit in volume. A
similar relation can also be obtained with a P-V-T relation explicit in the pressure.
The integration can be carried out, if a suitable equation of state is available for the
1
1
lnE n
E E E E E E
i in
i
i
i
Gg U TS Pv h Ts RT x
N
γ=
=
= = − + = − = ��
1
ln
kK
E En
E
j i
ij i x ix j
g gg x
x x
δ δγ
δ δ=≠≠
� � � �= + −� � � �� � � �� �
�
0
1exp
P
i i
RTv dP
RT Pϕ
� �� �= −� �� �
� �� �
24 Chapter 2
gaseous mixture or if experimental P-V-T data of the mixture are available. More
details on the equation of state approach are given in Section 2.4.
2.4 Equations of state
In the equation of state method (EOS), the same equation is used for both the vapor
phase as the gas phase. Most of the thermodynamic properties can be calculated
for pure components, if the P-V-T relation or equation of state is known. In 1873 van
der Waals developed his equation of state consisting of a repulsive and an
attractive term:
Equation 25
Parameter a is a measure for the attractive forces between the molecules and
parameter b is the covolume occupied by the molecules. These parameters can be
estimated from the critical properties and accentric factor of the specific component.
Numerous modifications to this equation have been developed. The Redlich-Kwong
equation of state is given below:
Equation 26
For highly polar components the predictions are not good and modifications have
been proposed in literature. Schwarzentruber et al. [25] adapted the RK model by
introducing additional parameters in the attractive temperature dependent term.
These additional parameters can be determined for each component by fitting the
EOS to experimental vapor pressure data for polar components; they are set to zero
for non-polar components.
The equation of state can be extended to mixtures by using appropriate mixing
rules, which relate the properties of the pure components to the real mixture. The
simplest mixing rule is the linear mixing rule, which is, however, seldom accurate.
2
RT aP
v b v= −
−
( )
( )
RT a TP
v b v v b T
= −− +
Thermodynamic models 25
The most commonly used mixing rule is from Van der Waals. The equations for the
van der Waals mixing rule are given in Equation 27:
Equation 27
The binary interaction parameter kij has to be determined by using a suitable fitting
procedure with experimental data on the binary mixture. This mixing rule is suitable
for many different mixtures, in particular hydrocarbons. However, mixtures
containing a polar component cannot be modeled accurately. Huron and Vidal [13]
have suggested a method for deriving mixing rules for equation of state models
using an excess Gibbs energy expression. In this method three major assumptions
have been made:
• The excess Gibbs energy calculated from an equation of state at
infinite pressure equals an excess Gibbs energy calculated from a
liquid activity coefficient model;
• The covolume parameter b equals the volume V at infinite
pressure;
• The excess volume is zero. An advantage of this Huron-Vidal
mixing rule is that it can easily be converted for non-polar binary
systems (i.e. hydrocarbons) to the van der Waals mixing rule by a
proper choice of the parameters.
The fugacity coefficient of a mixture can be calculated from the frequently used
equation:
Equation 28
( )1
2
i j ij ij i j ij
i i
i j
i j ij ij
i j
a x x a a a a k
b bb x x b b
= = −
+= =
��
��
0
ln ln
P V
i i
i i
RT nRTRT V dP P dV RT Z
n V n V
δ δϕ
δ δ∞
� � � �= − = − −� � � �
� � � �
26 Chapter 2
1
1
2
n
i i
i
I m z
=
= �
2.5 Electrolyte solutions
The models above are only applicable to molecular systems. In acid gas treating
processes where ions are formed in the liquid, non-idealities occur which cannot be
handled by molecular models. The electrostatic interactions which occur in the liquid
are strong and they are significant over long distances. In this section the different
electrolyte modifications are described for both the excess Gibbs energy and the
equation of state models.
2.5.1 Debye-Hückel approach
When traditional activity-coefficient models are used for calculation of
thermodynamic properties of electrolyte systems, it appears that extensive
modifications are needed to get satisfactory results. The reason is that electrolyte
solutions depend on both long-range electrostatic attractions and repulsions and on
short-range interactions between ions and between ions and molecules.
The first researchers that were able to predict these electrolyte interactions were
Debye and Hückel [6]. They derived an expression for the activity coefficient of an
electrolyte solution based on classical electrostatics. They considered the ions as
isolated point charges in a continuous dielectric solvent, were the ionic strength is
given by the following expression:
Equation 29
This leads to the so-called Debye-Hückel limiting law:
Equation 30
From this equation it can be seen that the activity of a strong electrolyte in a dilute
solution depends on the ionic strength I, the ion charges involved, the solvent
dielectric constant �r and the solvent molar density �s. Predictions of this model are
3/ 222
2 1/ 2ln (2 )8
A
i i s
o r
NeA z I A
RTγ γ
γ ρε ε π
� �= = � �
� �
Thermodynamic models 27
good for dilute electrolytes, however prediction at normal industrial ionic strengths is
poor. The equation only applies to solutions with an ionic strength up to 0.01 molal
(mole / kg solvent). In Figure 1 a comparison of activities calculated from the
Debye-Hückel model with experimental data is presented for some strong
electrolyte solutions.
Figure 1 Mean ionic activity coefficient as function of concentration for different
aqueous electrolytes. Solid lines are experimental data; dashed lines are
calculated from the Debye-Hückel limiting law. (Robinson and Stokes
[24])
From this figure it can be seen that the Debye-Hückel limiting law always predicts
negative deviation from experimental data. Guntelberg [10] has extended the model
to higher concentrations of 0.1 mol kg-1
by postulating the following relation for the
activity coefficient:
Equation 31
As mentioned before, the Debye-Hückel law only gives good results at
concentrations much lower than found in industry. The main reason for this is that
2
ln1
i
i
A z I
I
γγ =
+
28 Chapter 2
only long range interactions are incorporated in the Debye-Hückel model. This
assumption is only true at very low concentrations, because at low concentrations
the distance between the ions is in general far enough to neglect short range
interactions. However at more concentrated solutions short-range interactions, like
ion-molecule and molecule-molecule become significant.
The Debye-Hückel model has been improved by Guggenheim [9]. He recognized
that a drawback of the Debye-Hückel model was the inability to take into account
differences between several electrolytes of the same charge. Guggenheim added
an additional term to account for binary interactions. This resulted in the following
equation for an electrolyte solution with cation c and anion a:
Equation 32
Here �a and �c are the numbers of anions and cations in the electrolyte and c,a is
the interaction coefficient for the cation – anion interaction. With this model it was
possible to predict the activities of electrolyte solutions up to 0.1 M.
Pitzer [19] has developed one of the most used models for electrolyte solutions. He
uses a virial extension of the Debye-Hückel equation. The model has some
theoretical basis, but is partly empirical. It uses an excess Gibbs energy:
Equation 33
Here ws is the solvent molar mass, f(I) depends on the ionic strength, temperature
and pressure and represents the long-range electrostatic forces including the
Debye-Hückel limiting law, ij(I) represents the short range binary interaction
between two ion particles in the solvent, while �ijk is the tertiary interaction
coefficient for ion i, j and k. The activity coefficient of ion i (�i) is given by the
following equation:
Equation 34
, , ,
2 2ln
1
c a c a
c a c a a c a c
a cc a c a
A z z Im m
I
γ ν νγ β β
ν ν ν ν= + +
+ ++� �
1( ) ( ) ...
E
s i j ij i j k ijk
i j i j ks
Gw f I n n I n n n
RT nλ= + + Λ +�� ���
2,
,
, ,
( )( )ln 2 ( )
2 2
3
i ji i
i j j j k
j j k
i j k j k
j k
d Iz zdf Ii I m m m
dI dI
m m
λγ λ= + +
+ Λ
� ��
��
Thermodynamic models 29
The Pitzer equation has proved to be reliable for electrolyte concentrations up to
approximately 6 molal.
The Pitzer model has been extended by Chen et al. [4] by adding a molecular
contribution to the excess Gibbs energy of the Pitzer model. The model includes
two contributions for long range and short range interactions. The long range
interactions are described with the Pitzer model and the short range interactions are
characterized by the local composition concept originally developed for non-
electrolyte systems. The activity coefficient of an ion is calculated by summation of
the Pitzer term and a NRTL term as described by Renon and Prausnitz [23]. This
model has been tested successfully for both strong and weak electrolytes.
2.5.2 Mean Spherical Approximation approach
Another way of describing non-idealities in electrolyte solutions is based on the
mean spherical approximation (MSA) theory developed by Blum [2]. In contrast to
the Debye-Hückel approach, no solvent molecules are present in the MSA model,
but the solvent is represented by a dielectric medium. The ions are immersed in the
solvent and are represented as charged spheres of different sizes. The interaction
potential between two ions is described as follows:
Equation 35
Here zi and zj are the charges of ions i and j, D is the dielectric constant, rij is the
distance between the two ions and �ij is the average collision diameter of ions i and
j. The first MSA models were primitive, assuming equal sizes for cations and
anions. Planche and Renon [20] used the MSA theory to describe electrolyte and
polar systems with a Helmholz Free energy expression. With their model
experimental data up to a molality of 6 could be described.
ij ij
i j
ij ij
ij
U r
z zU r
Dr
σ
σ
= +∞ ≤
= ≥
30 Chapter 2
0
2 3(1 )
i j ij
i jSR
n n WA A
RT υ ε
−� �= −� �
−� ���
3
36
i i
i
nn σπε
ν= �
Fürst and Renon [8] developed a model for electrolyte solutions based on an
equation of state in combination with the MSA theory [20]. The model is based on
the ScRK-EOS (a modified Redlich-Kwong-Soave equation) and two additional
terms are added to incorporate the electrolyte interactions. This model is based on
an expression for the Helmholz free energy instead of the Gibbs free energy used in
the development of the GE-models. However, the Helmholz energy function is
composed as a sum of independent contributions due to the different interactions in
the same manner as implemented in the GE-models. According to Fürst and Renon
the total excess Helmholz energy can be calculated by the equation below:
Equation 36
• Molecular repulsive interactions (RF);
• Short rang molecular interactions (SR1);
• Short-range ion-ion and ion-molecule interactions (SR2);
• Long range ion-ion interactions (LR);
• Born term.
The first two terms (RF and SR1) described by a molecular equation of state, while
the additional ionic interactions (SR2, LR and BORN) are described with the above
mentioned MSA model. The short range ionic interaction term (SR2) is presented by
the following relation:
Equation 37
where at least one i or j is an ion and Wij is an ion-ion or ion-molecule interaction
parameter. �3 is calculated by the following formula:
Equation 38
1 2
R R R R R R
RF SR SR LR BORN
A A A A A A
RT RT RT RT RT RT
� � � � � � � � � � � �= + + + +� � � � � � � � � � � �
� � � � � � � � � � � �
Thermodynamic models 31
22 3
0
4 1 3
i iLR
iLR i
A A n Z
RT N
α ν
π σ π
− Γ Γ� �= +� �
+ � ��
2
2 241
i i
LR
i i
n ZNα
υ σ
� �Γ = � �
+ � ��
22
0
LR
e N
DRTα
ε=
( ) 3
3
1 "1 1
1 " / 2s
D Dε
ε
� �−= + − � �
+� �
i i
i
s
i
i
n D
Dn
=
��
(1)(0) (2) (3) 2 (4) 3
i
dD d d T d T d T
T= + + + +
The summation is over all species i and �i is the molecular or ionic diameter. The
long-range ion-ion interaction term is given by the following relation:
Equation 39
The shielding parameter is given implicitly by the following equation:
Equation 40
Equation 41
where �0 is the dielectric permittivity of free space. The dielectric constant D is
calculated from the equation below:
Equation 42
In this equation �”3 is equal to �3 as defined in Equation 38 above, but the sum is
taken only over the ions present in the system. The solvent dielectric constant is
given by:
Equation 43
The summation is only over the molecular components. The pure component
dielectric constant is assumed to be temperature dependent (see Equation 44). No
interaction parameters are necessary for the calculation of the dielectric constant.
Equation 44
In this model the standard state of the long-range (LR) term is not equal to the
standard state of the other terms (RF, SR1 and SR2) of the equation of state.
32 Chapter 2
22
0
*
0
11
4
i i
iBORN s i
A A n ZNe
RT RT Dπε σ
� �−� �= −� �� �
� � � ��
Therefore, an additional “Born” term is added to the Helmholz energy contributions.
This Born term is given by:
Equation 45
Only the interactions between cations and molecules Wcm and cations and anions
Wca are taken into account in the E-EOS model. Anion-anion and cation-cation
interactions are neglected, because the forces between like ions are repulsive. Also
the anion-molecule interactions are neglected as the solvation of anions is much
less, than that of the cations. In this model it is assumed that the ionic binary
interaction parameters Wij are not temperature dependent.
2.6 Discussion of the models
In this section the different thermodynamic models described are compared and
discussed qualitatively.
2.6.1 Semi-empirical models versus rigorous models
The semi-empirical models, that do not use activity coefficients but apparent
equilibrium constants, are able to predict the experimental acid gas pressure as a
function of liquid loading rather well. The models can be developed and used easily.
The required computer power and time are negligible compared to those of the
rigorous thermodynamic models described in this chapter. However, VLE prediction
is poor outside the range of experimental data where the apparent equilibrium
constants are fitted. Also speciation of the liquid (splitting the fluid into its species)
cannot be done accurately with these (semi)-empirical models. The liquid speciation
plays an important role in the calculation of mass transfer in absorbers and
desorbers of gas treating plants. Because of these drawbacks detailed mass
transfer calculations require more advanced models.
Thermodynamic models 33
2.6.2 Excess Gibbs energy models versus electrolyte equations
of state
Two different approaches which are capable of calculating liquid speciation are the
excess Gibbs energy �-� models and the electrolyte equation of state (E-EOS). The
excess Gibbs energy models are commonly used in the gas treating industry; the
electrolyte equation of state approach is a new development in this area.
Different equations for liquid and vapor phase:
The vapor and the liquid phase are described differently in the �-� models. The
vapor phase is described with an equation of state, while the liquid phase is
described with an activity model. At low pressure this has no negative effect.
However, at elevated pressures (i.e. in absorbers of natural gas plants), the critical
conditions of the fluid may be approached or exceeded. In these cases, the
difference between liquid and vapor becomes smaller and may even disappear. A
different approach of the liquid and the vapor can result in inconsistencies. In the
equation of state approach, where both phases are described with the same
equation this inconsistency does not exist.
Influence of pressure:
In the classical excess Gibbs energy models it is normally assumed that the excess
volume is zero (v=�xivi) and therefore GE=A
E. This assumption makes these models
pressure independent, because
,
E
E
T n
GV
P
δ
δ
� �=� �
� �. For normal low pressure
applications the influence of pressure on the thermodynamic properties is negligible.
However, when models at elevated pressure have to be used, a correction factor for
the fugacity in the liquid phase has to be incorporated. The fugacity of the liquid
phase is calculated according the following formula:
Equation 46
exps
i
P l
l s s i
i i i
P
v dPf P
RTϕ
� �� �=� �� �
34 Chapter 2
Superscript s means at saturation conditions. From Equation 46 it can be seen that
the fugacity of a pure component in the liquid phase can be estimated by the
saturation pressure of that component. Two corrections to this approximation may
be required:
• If the saturated vapor has a non-ideal behavior the fugacity coefficient of
the gas phase �s is needed;
• The exponential term is called the Poynting factor. This term allows one to
calculate the fugacity at pressure P instead of that at pressure Pis. The
Poynting contains the liquid volume of component i at temperature T which
is a function of pressure P. However when the pressure P is much lower
than the critical pressure, the liquid density is independent of pressure and
the following relation is normally used:
Equation 47
Normally the influence of these corrections on the liquid fugacity can be neglected.
However, for high temperatures, the assumption that �si = 1 is not correct. Neither is
the assumption that the liquid phase is incompressible correct for high pressures. In
equations of state a Poynting factor correction is not required, because the liquid
fugacities are calculated using the equation of state. Therefore, for high pressures
such as in absorbers of gas treating plants, the assumption that the liquid phase is
incompressible may introduce erroneous results in the calculated liquid fugacities
when excess Gibbs energy models are used.
In Figure 2 the CO2 partial pressure is presented as a function of the acid gas liquid
loading at different partial pressures of methane (6.9 < PCH4 < 69 bar). A
comparison of experimental data with predictions of the electrolyte equation of state
are given in this figure. The influence of pressure of methane partial pressure can
be clearly seen from this picture. A higher partial pressure of methane results in a
( )exp
l s
i iv P P
RT
� �−� �� �� �
Thermodynamic models 35
higher acid gas partial pressure, so the acid gas solubility decreases significantly
with increasing methane partial pressure.
0.10
1.00
10.00
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35
Liquid loading [mole CO2 / mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
6.9 bar (experimental)
6.9 bar (E-EoS model)
34.5 bar (experimental)
34.5 bar (E-EoS model)
69 bar (experimental)
69 bar (E-EoS model)
Figure 2 Solubility of CO2 in 35 wt.% MDEA at 283 K
Usually, VLE experiments are carried out without inert components or with low
pressure nitrogen as inert. However, from Figure 2 it can be seen that influence of
the presence of a nonreacting component (in this case methane) can have a
significant influence on the acid gas solubility. From this picture it can be seen that
the influence of methane on the acid gas solubility can be predicted quite
satisfactorily by the electrolyte equation of state.
Non condensables:
In excess Gibbs energy models non condensable components such as CO2, H2S
and hydrocarbons are normally treated as Henry components. Therefore, the Henry
coefficient (the gas solubility of all non condensable components in the liquid) needs
to be determined. Because these Henry coefficients depend on the liquid
composition, a suitable mixing rule has to be determined. This mixing rule
introduces additional inaccuracies in the model, because no fundamental mixing
36 Chapter 2
rule is available for Henry coefficients. In the electrolyte equation of state Henry
coefficients are not required as input parameters, because the gas solubility is
directly calculated from the E-EOS. Moreover, when data on Henry coefficients are
available, a comparison with the outcome of the E-EOS model gives additional
information on the accuracy and reliability of the model.
2.7 Conclusion
The selection of a suitable thermodynamic model for the gas treating industry
depends strongly on the requirements for the model. If only total solubility of a
known system needs to be calculated or computer calculation time is limited, the
semi-empirical models may be sufficient. In these models the system is considered
to be ideal, so no activities and fugacities are used. It must be noted that this
approach only leads to reliable results, when it interpolates in the range of the
experimental area.
However, when detailed mass transfer calculations are required, the liquid
composition becomes an important consideration and more rigorous VLE-models
need to be used. The selection between excess Gibbs energy models �-� and
electrolyte equations of state is based on the required application. For high pressure
applications an E-EOS is better suitable for describing the influence of nonreacting
components such as hydrocarbons. In this chapter it has been shown that an E-
EOS can predict the influence of the partial pressure of methane on the acid gas
solubility, however, more research is required in this area to describe the influence
of other non-reacting components.
At the moment the VLE models have been developed by fitting these models to
experimental data containing the total acid gas solubility as function of the acid gas
partial pressure. Information about the actual speciation in the liquid phase is hardly
available. The accuracy and reliability of the rigorous VLE models can be improved
significantly, when this speciation in the liquid phase can be determined
Thermodynamic models 37
quantitatively, for example by means of ion selective electrodes, pH measurements,
conductivity measurements or NMR spectroscopy (Nuclear Magnetic Resonance).
So development of rigorous VLE models should be focused on this subject.
List of symbols
Parameters
a Interfacial area; attractive parameter in EOS
A Helmholtz energy
b Covolume parameter in EOS
D Dielectric constant
DEA Diethanol amine
E Electron charge
(E)EOS (Electrolyte) Equation Of State
f Fugacity
G Gibbs energy
H Henry constant
I Ionic strength
kg Gas side mass transfer coefficient
ki,j Binary interaction parameter
kl Liquid side mass transfer coefficient
m Molality
MDEA N-methyldiethanolamine
MEA Monoethanolamine
n Number of moles
NA Number of Avogadro
P Pressure
Q Heat
R Gas constant
rij Distance between ion i and j
38 Chapter 2
S Entropy
T Temperature
U Internal energy
V Total volume
v Molar volume
VLE Vapor Liquid Equilibrium
W Work
x Liquid mole fraction
y Vapor mole fraction
Z Compressibility
z Ion charge
Greek symbols
� Acid gas liquid loading
� Activity coefficient
� Permittivity
� Chemical potential
� Number
� Molar density
� Collosion diameter
� Fugacity coefficient
Sub/super-scripts
a Anion
c Cation
e Equilibrium
i,j Component i,j
t Total
Thermodynamic models 39
0 Reference state
l Liquid
r Residual properties
v Vapor
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40 Chapter 2
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Thermodynamic models 41
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42 Chapter 2
43
Chapter 3
Solubility of Carbon Dioxide in
Aqueous N-methyldiethanolamine
Abstract
In this chapter the electrolyte equation of state proposed by Solbraa (E. Solbraa,
Ph.D. thesis Norwegian University of Science and Technology (2002)) is studied
and improved to describe the solubility of carbon dioxide in aqueous solutions of N-
methyldiethanolamine quantitatively. In this equation both the vapor and the liquid
are described by an equation of state. The molecular part of the equation is based
on Schwarzentruber’s modification of the Redlich-Kwong equation of state (J.
Scharzentruber, H. Renon, S. Watanasiri, Fluid Phase Eq., 52 (1989) 127-134) with
the Huron-Vidal mixing rule (M.J. Huron, J. Vidal, Fluid Phase Eq., 3 (1979) 255-
271). Three ionic terms are added to this equation – a short-range ionic term, a
long-range ionic term (MSA) and a Born term. The thermodynamic model has the
advantage that it reduces to a standard cubic equation of state if no ions are
present in the solution, and that publicly available interaction parameters used in the
Huron-Vidal mixing rule can be utilized. In this chapter binary molecular - and ionic
interaction parameters are studied and optimized. With the updated model it is
44 Chapter 3
possible to describe both the low- and high pressure vapor-liquid-equilibrium of the
MDEA-H2O-CO2-CH4 system satisfactorily.
3.1 Introduction
Acid components like CO2 and H2S are often removed to a certain extent from
natural and industrial gas streams. The most commonly used systems remove
these gases with a reactive absorption liquid, i.e. an aqueous alkanolamine solution.
The acid gas will be partly converted to non-volatile ionic species by the basic
amine and will be partly dissolved physically in the liquid. For a robust design the
acid gas solubility (VLE data), the reaction rate and the mass transfer properties
need to be known accurately. In this chapter experimental solubility data available in
the literature are interpreted with an electrolyte equation of state (E-EOS) model for
the system MDEA-H2O-CO2-CH4. MDEA is a commonly used alkanolamine in the
gas treating industry. It is a cheap chemical, it is stable and the loaded solvent has
a low heat of regeneration. With the E-EOS thermodynamic model all molecular and
ionic concentrations for MDEA-H2O-CO2-CH4 can be calculated at chemical
equilibrium conditions.
In literature many models are presented to predict the acid gas solubility in
alkanolamine systems. These models can be divided in three categories:
• Empirical models like that of Kent-Eisenberg [2]. The Kent-Eisenberg model
is based on a chemical reaction equilibrium in the liquid. All activity and
fugacity coefficients are assumed to be equal to unity and both the
equilibrium constant of the amine protonation reaction and the carbamate
formation reaction are used as fitting parameters in the model. Applicability
outside the validity range is limited. This model is commonly used by
process engineers because the complexity and required computational
effort are low;
CO2 solubility in aqueous MDEA 45
• Excess Gibbs energy models. In these models a term, for electrostatic
forces caused by the presence of ions in the liquid, is added to the
molecular Gibbs free energy models like NRTL. This additional term is
normally based on the Debye and Hückel expression. Approaches based
on an excess Gibbs energy are presented by: Desmukh-Mather [3], Clegg-
Pitzer [4] and Austgen et al. [5]. The vapor is described with a suitable
equation of state;
• Equation of state models (EOS). In this approach both the liquid and the
vapor are described by an equation of state. Additional electrolyte terms for
the forces resulting from the presence of ions are added. These models are
rather new for the prediction of acid gas solubility in alkanolamine solutions
(Fürst and Planche [6], Solbraa [7], Derks et al. [8]).
A more detailed comparison of these thermodynamic models used in the gas
treating industry is presented by Huttenhuis and Versteeg [10].
In this chapter experimental data for CO2 will be interpreted with an electrolyte
equation of state. This model selection is based on the following motivation:
• EOS models apply the same description to liquid and gas;
• The model can describe the condensate and amine equilibria (VLLE) in a
consistent way;
• The model is thought to allow extrapolation;
• Prediction at the high pressures found in the natural gas industry, is
expected to be more reliable compared to other thermodynamic models;
• The model can be extended to systems where different kinds of inert
components like hydrocarbons are present;
• The model reduces to a standard cubic equation of state if no ions are
present in the solution, and so enables a consistent overall natural gas
process simulation.
46 Chapter 3
1 2
1 2 3 4 5
R R R R R R
RF SR SR LR BORN
A A A A A A
RT RT RT RT RT RT
� � � � � � � � � � � �= + + + +� � � � � � � � � � � �
� � � � � � � � � � � �
3.2 The electrolyte equation of state
3.2.1 General
The experimental results are interpreted with an electrolyte equation of state (E-
EOS), originally proposed by Fürst and Renon [9]. In this model the same
equations, based on an equation of state, are used for the liquid and vapor. These
EOS models are expected to be superior in representing the thermodynamic
properties outside the experimentally tested region. Also, they are thought to allow a
more reliable calculation of the speciation of the components in the liquid. An
accurate prediction of the speciation is important for mass transfer calculations.
Moreover, the solubility of physically dissolved hydrocarbons (i.e. methane) can be
calculated in a thermodynamically consistent way. This hydrocarbon solubility is an
important parameter for the correct design of high pressure gas treating equipment.
The model is based on a Helmholtz free energy expression. The Helmholtz energy
is given below and is defined as the sum of five contributions:
Equation 1
The first two (molecular) terms are the terms obtained from the molecular equation
of state and the other terms are added to allow for the presence of electrolytes in
the system.
In Figure 1 an overview is given of the types of interaction parameters in the E-EOS
for the system MDEA-CO2-H2O-CH4 and how these parameters are determined. At
the bottom level, independent pure component molecular and ionic parameters are
given. The molecular interaction parameters are determined from the binary
systems by fitting them to the experimental VLE database derived from open
CO2 solubility in aqueous MDEA 47
( )
RT aP
v b v v b= −
− +
literature on the systems CO2-MDEA-H2O and CO2-MDEA-H2O-CH4. More details
on the model and its parameters are described in the following subsections.
CO2 Water MDEA
CO2 - Water
CO2 - MDEA
Water - MDEA
HCO3- MDEAH+OH-CO3--CH4
CH4 - CO2
CH4-Water
CH4-MDEA
CO2 – MDEA - Water - CH4
Pure component parameters
Molecular interactions parameters
Ionic interaction parameters
Figure 1 Overview of the interactions involved in the E-EOS model
3.2.2 The pure component model
The first term of the Helmholtz free energy contributions accounts for molecular
repulsive forces (RF) and the second term for the short-range (attractive)
interactions (SR1). The molecular part of the model is based on a cubic equation of
state (Schwarzentruber’s [1] modification of the Redlich-Kwong-Soave EOS (ScRK-
EOS) with a Huron-Vidal [11] mixing rule).
This ScRK-EOS is described by the following formulae:
Equation 2
48 Chapter 3
( )1
2
i j ij ij i j ij
i i
i j
i j ij ij
i j
a x x a a a a k
b bb x x b b
= = −
+= =
��
��
( )
( ) ( ){ ( ) }
( ){ }
( )
2
1/3
1/3
22
1 2 3
2
2
1 2 3
1( )
9(2 1)
(2 1)
3
( ) 1 ( ) 1 1 1 1
( ) exp 1 1
( ) 0.48508 1.55191 0.15613
1 1/
1 ( ) / 2 1
c
R
c
C
C
R R R R R R
d
R r R
RTa T
P
RTb
P
T m T p T p T p T for T
T c T for T
m
c d
d m p p p
α
α ω
α
ω ω ω
ω
=−
−=
= + − − − + + <
�= − >�
= + −
= −
= + − + +
Equation 3
Using the Schwarzentruber modification of the RKS equation, it is also possible to
calculate the vapor-pressure curve as function of temperature for polar (non-ideal)
components. Parameters p1, p2 and p3 are fitting parameters and are determined by
regressing the model against the experimental vapor pressure data.
3.2.3 Mixing rules
The equation of state can also be used to predict physical and thermodynamic
properties for mixtures of components. The parameters applicable to pure
components like ‘a’ and ‘b’ are then determined via a mixing rule. The most simple
mixing rule is a linear mixing rule; however, for more accurate predictions, the
mixing rule developed by van der Waals is used:
Equation 4
Here kij is a fitting parameter.
CO2 solubility in aqueous MDEA 49
1 ln 2
En
i
mix mix i
i i
a Ga b x
b
∞
=
� �� �= −� �� �� �� �� �
�
1
1
1
exp( )
exp( )
n
ji j j ji jiE n
j
i n
i
k k ki ki
k
b xG
xRT
b x
τ α τ
α τ
=∞
=
=
−
=
−
��
�
ji ii
ji
g g
RTτ
−=
( ' ' ) ( " " )
( ' ' ) ( " " )
ij jj ij jj ij jj
ji ii ji ii ji ii
g g g g T g g
g g g g T g g
− = − + −
− = − + −
When components with substantially different structures have to be described the
van der Waals mixing rule is not reliable, Huron and Vidal [11] have proposed a
mixing rule based on excess Gibbs energy models. In this mixing rule the attraction
parameter of the mixture (amix) is calculated in a way different from the van der
Waals method. With this mixing rule better predictions can be obtained for polar,
highly non-ideal mixtures:
Equation 5
GE� is the excess Gibbs energy at infinite pressure; it can be calculated with a
modified NRTL mixing rule:
Equation 6
�ji is a non-randomness parameter, which takes into account that the mole fraction
of molecule i around molecule j may deviate from the total mole fraction of molecule
i in the system.
Equation 7
gji is an energy parameter describing the interaction forces between molecule i and
j. In the present approach it is assumed that the g-parameters are temperature
dependent according to:
Equation 8
50 Chapter 3
mix m m ion ion
m ion
b x b x b= +� �
An additional advantage of this Huron-Vidal mixing rule is that it can easily be
converted for non-polar binary systems (i.e. hydrocarbons) to the van der Waals
mixing rule by proper choice of parameters. In this thesis the non-polar binary
mixtures are modelled with the van der Waals mixing rule and the polar, non-ideal
binary mixtures with the Huron-Vidal mixing rule. In this model the linear mixing rule
is used for the co-volume parameter bmix, while the presence of ions is included:
Equation 9
The molecular co-volume (bm) is calculated from the critical properties and the ionic
co-volume (bion) is calculated from the ionic diameter. The pure component
parameters of the E-EOS model used in this chapter are presented in Table 1.
CO2 MDEA H2O CH4 HCO3-
CO32-
MDEAH+
OH-
M [gr mole-1
] 44.01 119.16 18.02 16.04 61.00 59.98 120.16 17.00
TC [K] 304.2 677.0 647.3 190.6
PC [bar] 74.0 38.8 220.9 45.9
� [-] 0.224 1.242 0.344 0.011
p1 0.0336 0.5213 0.0740 0.0145
p2 -1.3034 -1.1521 -0.9454 1.7953
p3 0 -0.0139 -0.6988 -4.2300
� [10-10
m] 2)
3.94 1) 4.50 2.52
1) 3.17 3.12 1)
3.7 1) 4.50 3.52
1)
d(0) 2) 2.00 8.17 -19.29 2.00
d(1) 2) 0 8.989E+03 2.981E+04 0
d(2) 2) 0 0 -1.968E-02 0
d(3) 2) 0 0 1.320E-04 0
d(4) 2) 0 0 -3.110E-07 0
1) All parameters are based on Solbraa [7] except those marked with
1), which are based on Vallée et al.
[12]
2) These pure component parameters are used in the electrolyte part of the equation of state as
discussed in the next sections
Table 1 Pure component parameters
CO2 solubility in aqueous MDEA 51
22 3
4 1 3
ion ionR LR
ionLR ion
x ZA v
RT N
α
π σ π
Γ Γ� �= − +� �
+ � ��
2 3(1 )
i j ijR
i jSR
x x WA
RT v ε
� �= −� �
−� ���
3
36
i i
i
xN
v
σπε = �
2
2 241
ion ion
LR
ion ion
x ZN
vα
σ
� �Γ = � �
+ � ��
22
0
LR
e N
DRTα
ε=
3.2.4 Electrolyte interactions
To describe the interactions caused by the presence of ions in the system the
following terms were added to the (molecular) equation of state:
• SR2 – a short-range ion-ion interaction term;
• LR – a long range ion-ion interaction term;
• A Born term, a correction term for the standard state of the ions.
The short range ionic interaction term is calculated using:
Equation 10
where at least one i or j is an ion and Wij is an ion-ion or ion-molecule interaction
parameter. The packing factor �3 is calculated by the following formula:
Equation 11
with a summation over all species present, while �i is the molecular or ionic
diameter respectively.
The long-range ion-ion interaction term is given by:
Equation 12
The shielding parameter is given implicitly by:
Equation 13
Equation 14
52 Chapter 3
(1)(0) (2) (3) 2 (4) 3
i
dD d d T d T d T
T= + + + +
( ) 3
3
1 "1 1
1 " / 2s
D Dε
ε
� �−= + − � �
+� �
mol mol
mol
s
mol
mol
x D
Dx
=
��
where �0 is the dielectric permittivity of free space. The dielectric constant D is
calculated using:
Equation 15
In this equation �”3 is equal to �3 as defined in equation 11; however, the summation
is only over the ions present in the system.
The solvent dielectric constant is given by:
Equation 16
The summation is only carried out for the pure molecular components. The pure
component dielectric constant is assumed to be temperature dependent (Equation
17). No interaction parameters are necessary for the calculation of the dielectric
constant.
Equation 17
In the model described above the standard state of the long-range (LR) term is not
equal to the standard state of the other terms (RF, SR1 and SR2) of the equation of
state. The following standard states are used in the model:
• Ionic standard state in the solvent mixture at unit mole fraction and the
system temperature and pressure (for LR term);
• Ideal gas state at unit mole fraction and system temperature and 1 bar (for
RF, SR1 and SR2 term).
These two different standard states cause a discrepancy. To prevent this an
additional “Born” term is added to the equation of state. This term is given by
Equation 18:
CO2 solubility in aqueous MDEA 53
22
*
0
11
4
i iR
iBORN s i
x ZA Ne
RT RT Dπε σ
� �� �= −� �� �
� � � ��
ln lnx
BK A C T
T= + +
1
2 32K
H O H O OH+ −
←⎯→ +
2
2 2 3 32K
H O CO HCO H O− +
+ ←⎯→ +
3 2
2 3 3 3
KH O HCO CO H O
− − ++ ←⎯→ +
4
2 3
KH O MDEAH MDEA H O
+ ++ ←⎯→ +
Equation 18
In this thesis (as in previous work by Fürst and Renon [9]) only the interactions
between cations and molecules (Wcm) and cations and anions (Wca) are taken into
account. Other interactions are not incorporated. The anion-anion and cation-cation
interactions are thought to be small, because of repulsive forces and the solvation
of anions is small compared that of the cations. In this model it is assumed that the
ionic binary interaction parameter (Wij) is not temperature dependent.
3.2.5 Chemical reactions
An alkanolamine-acid gas system is a reactive absorption system, so chemical
reactions have to be incorporated in the model. In the CO2-MDEA-H2O-CH4 system,
the following chemical reactions take place:
Water dissociation:
Bicarbonate formation:
Carbonate formation:
MDEA protonation
The equilibrium constants (based on mole fractions) of these reactions are
correlated by the following equation:
Equation 19
The parameters for the equilibrium constants are given in Table 2.
54 Chapter 3
KX A B C T [K] Reference
K1 132.899 -13445.9 -22.4773 273-498 Posey and Rochelle [13]
K2 231.465 -12092.1 -36.7816 273-498 Posey and Rochelle [13]
K3 216.049 -12431.7 -35.4819 273-498 Posey and Rochelle [13]
K4 -77.262 -1116.5 10.06 278-423 Appendix A [15]
Table 2 Parameters for the calculation of chemical equilibrium constants of the
system CO2-MDEA-H2O
K1, K2, K3 as used by Posey [13] have been compared with the chemical equilibrium
constants used by Kamps et al. [16]; the differences between these two are
negligible. K4 has been compiled in Huttenhuis et al. [15] from experiments carried
out by different research groups.
In this thesis all chemical equilibrium constants are defined in the mole fraction
scale with as reference state infinite dilution in water. Now all the relevant and
required equations and parameters have been specified and the model can be
finalized. In the model H3O+ is neglected, since at low to moderate loadings, the
solution is alkaline. The mole fraction of the following species are calculated: H2O,
OH-, CO2, HCO3
-, CO3
2-, MDEA, MDEAH
+ and CH4.
3.3 Model development
3.3.1 Former work
As described by Huttenhuis et al. [15] the agreement between the original model of
Solbraa [7] and the newly determined experimental data is not satisfactory.
Therefore modifications to the original EOS of Solbraa [7] have been carried out:
CO2 solubility in aqueous MDEA 55
• The experimental database used for the determination of the ionic
interaction parameter of MDEAH+ with the other species in the system has
been critically reviewed and updated;
• The dissociation constant of MDEA of the model has been changed,
because the value used previously does not agree with the experimentally
determined equilibrium constants in the literature.
Moreover, it appears that the physical solubility of the CO2 in the liquid, as
calculated by the model, is not in line with the experimental data (Huttenhuis et al.
[15]).
For a quantitative comparison of the model with experimental data the average
absolute deviation (AAD) and BIAS deviation are used:
,exp , ,exp ,
1 1,exp ,exp
1 1100% 100%
n n
i i calc i i calc
i ii i
y y y yAAD BIAS
n y n y= =
− −= ⋅ = ⋅� �
3.3.2 Chemical reactions
In the model developed by Solbraa [7], the species OH- and CO3
2- were not taken
into account. However, at very low CO2 liquid loadings (influence of OH--ions) and
higher MDEA concentrations and/or high CO2 liquid loadings (influence of CO32-
-
ions) these assumptions may lead to erroneous results. Therefore these two
species and the relevant interaction parameters have been incorporated in the E-
EOS. For the governing reaction equations and their equilibrium constants
reference is made to Section 3.2.5.
56 Chapter 3
3.3.3 Binary molecular interaction parameters
3.3.3.1 Overview
Before the quaternary system CO2-MDEA-H2O-CH4 can be simulated, the following
binary systems have to be studied and optimized:
• CO2-H2O: the Huron-Vidal binary interaction parameters for this system
have been found by fitting the parameters to experimental solubility data
(222 data points) of CO2 in water. This work was carried out by Solbraa [7];
• H2O-MDEA: in Solbraa’s original model 25 freezing point data of Chang et
al. [17] have been used to determine the Huron-Vidal interaction
parameters. In this chapter this experimental database is extended and
three additional literature sources have been added. New Huron-Vidal
interaction parameters have been determined with the changed database;
• CO2-MDEA: in Solbraa’s original model the Huron-Vidal interaction
parameters were determined by fitting them together with the ionic
interaction parameters of ternary reactive solubility data. Huttenhuis et al.
[15] have concluded that the calculated physical solubility of CO2 in MDEA
does not agree with experimental data, so the binary interaction parameter
of this system was critically re-evaluated;
• CH4-CO2: the van der Waals mixing rule is used for this non-polar system.
The interaction parameter kij is the same as that used in Solbraa’s original
model and is taken from Prausnitz et al. [18] and Reid et al. [19];
• CH4-H2O: the Huron-Vidal binary interaction parameters for this system
were found by fitting the parameters to experimental solubility data (400
data points) of CH4 in water and water in CH4. This work was carried out by
Solbraa [7];
• CH4-MDEA: in the Solbraa version of the model this molecular interaction
parameter was determined by using it as a fitting parameter (together with
the ionic fitting parameter MDEAH+-CH4) for the ionic system MDEA-H2O-
CO2 solubility in aqueous MDEA 57
CO2-CH4. In the new approach this interaction parameter is determined
from experimental data of the ternary molecular system MDEA-H2O-CH4.
3.3.3.2 H2O-MDEA
In Solbraa’s original model freezing point data (25 data points) of Chang et al. [17]
in a relatively small temperature range (262-273 K) have been used to determine
the Huron-Vidal interaction parameters. In this chapter three additional literature
sources have been added so that a higher temperature range was covered (262-
460 K), Xu et al. [20] (34 VLE data points), Voutsas et al. [21] (27 VLE datapoints)
and Posey [14] (19 excess heat of mixing data points). As can be seen in Table 3
the deviations for the water-MDEA system are significantly reduced by the new
binary interaction parameters.
AAD [%] Reference Solbraa’s This work
Chang et al. [17] 1.5 0.25
Xu et al. [20] 2.5 3.1
Voutsas et al. [21] 7.4 3.3
Posey [14] 37.3 4.0
Table 3 Model predictions compared with experimental data for the MDEA-H2O
system
In Figure 2 the calculated activity coefficient for water in the H2O-MDEA system is
compared with the experimental data of Chang et al. [17]. As it can be seen from
this figure, the calculated activity coefficient in the new model is significantly
improved compared to Solbraa’s model, especially for the more concentrated
MDEA solutions.
58 Chapter 3
0.95
0.96
0.97
0.98
0.99
1
0 0.01 0.02 0.03 0.04 0.05 0.06 0.07 0.08 0.09 0.1
Mole fraction MDEA [-]
Wate
r acti
vit
y c
oeff
icie
nt
Chang et al. (1993)
Solbraa (2002)
This work
Figure 2 Activity coefficient of water in a MDEA-H2O mixture (263<T<273 K)
When molecular interaction parameters are fitted to binary data, sometimes multiple
sets of parameters are obtained. For the MDEA-H2O mixture two sets of Huron –
Vidal parameters (HV-I and HV-II) were obtained during the regression calculations.
In Table 4 the two sets of Huron-Vidal parameters are presented and the
thermodynamic consequences are further discussed:
HV-I HV-II
comp.i MDEA MDEA
comp.j H2O H2O
�ji [-] 0.208 0.270
�'gij [J mol-1
] -9148 33219
�'gji [J mol-1
] 6095 -46531
�''gij [J mol-1
K-1
] 42.35 -66.84
�g''ji [J mol-1
K-1
] -49.93 91.29
Table 4 Two sets of Huron-Vidal parameters for the MDEA- H2O system
CO2 solubility in aqueous MDEA 59
In Figure 3 and Figure 4 the calculated activity coefficient of H2O and MDEA is
presented for the two different sets of Huron – Vidal parameters as function of the
mole fraction water at 313 K.
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
mole fraction H2O [-]
acti
vit
y c
oefi
cie
nt
[-]
H2O [HV-I]
H2O [HV-II]
Figure 3 Calculated activity coefficient of water in a MDEA-H2O mixture at 313 K for
two different sets of Huron-Vidal parameters (HV-I and HV-II)
60 Chapter 3
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
mole fraction H2O [-]
acti
vit
y c
oefi
cie
nt
[-]
MDEA [HV-I]
MDEA [HV-II]
Figure 4 Calculated activity coefficient of MDEA in a MDEA-H2O mixture at 313 K
for two different sets of Huron-Vidal parameters (HV-I and HV-II)
From Figure 3 and Figure 4 it can be seen that the behaviour of both the MDEA and
the H2O activity coefficient is different for the two sets of parameters. For
commercial applications, the MDEA concentrations used result in values for the
mole fraction of water above 0.85, in this range the difference in the H2O activity
coefficient predicted by the two sets is negligible. However, two completely different
sets of activity coefficients are found for MDEA. When the HV-I parameters are
used, a minimum in the MDEA activity coefficient of 0.55 is predicted, while for the
HV-II parameters a continuously decreasing activity (with increasing water
concentration) is found. In dilute MDEA solutions the MDEA activity coefficients of
the two models differ by more than a factor of 5! The minimum in the MDEA activity
coefficient as function of concentration was also observed by Solbraa [7], Posey
[14], Lee [22] and Austgen [23]. However, Austgen concluded that a better model
representation of the ternary system (CO2-MDEA-H2O) is achieved by setting all
MDEA-H2O interaction parameters to zero instead of using the fitted parameters.
Austgen, however, could not give an explanation for this observation. Contrary to
CO2 solubility in aqueous MDEA 61
2
2 2
2
,
, . , .
,
CO water
CO aq MDEA N O aq MDEA
N O water
HH H
H= ⋅
the authors mentioned above, Poplsteinova et al. [24] calculated a continuously
decreasing MDEA activity coefficient (with increasing H2O concentration),
comparable with the model using parameters HV-II.
In the present study it was decided to use the HV-I parameters in the model,
because predictions of the MDEA activity coefficient of this model are in line with
most of the other authors. Also the predicted activity coefficient of water at infinite
dilution (pure MDEA) of the HV-I model is more in line with the other authors.
However, further work is required to generate more experimental data in the
commercially important MDEA concentrations range. Different types of data can be
used for the estimation of the Huron-Vidal parameters. However, it has been
demonstrated by Posey [14] that heat of mixing data and freezing point data are
more suitable for predicting the binary interactions for the MDEA-H2O system.
3.3.3.3 CO2-MDEA
In the original model, the Huron-Vidal interaction parameters were determined by
fitting them together with the ionic interaction parameters to ternary solubility data.
As discussed by Huttenhuis et al. [15], the physical solubility of CO2 calculated by
the model does not match the experimental data. The physical solubility of CO2 in
MDEA cannot be measured directly, because there are always trace amounts of
water present in pure MDEA. These small amounts of water will increase the CO2
solubility enormously, due to the chemical reaction which takes place. So for the
prediction of the physical solubility in aqueous MDEA, the CO2-N2O analogy is
widely accepted in the literature. This theory is based on the fact that CO2 and N2O
are similar molecules. The only difference is, that N2O only dissolves physically in
aqueous MDEA. According to the CO2-N2O analogy the Henry constant (physically
dissolved CO2) of CO2 in aqueous MDEA can be calculated using:
Equation 20
62 Chapter 3
So the physical solubility of CO2 in aqueous MDEA can be determined by
measuring the solubility of N2O in water and aqueous MDEA and the solubility of
CO2 in water. In this indirect way binary interaction parameters for MDEA-CO2 can
be obtained. For the solubility of CO2 and N2O in water the empirical correlation of
Jamal [25] has been compared with the relation presented by Versteeg et al. [26].
The solubilities predicted by both relations are comparable up to a temperature of
approximately 333 K. Above this temperature the Henry constant of N2O predicted
by Versteeg is higher than that calculated from the relation of Jamal. Therefore,
some additional experiments have been carried out to verify which relation is more
correct. Experimental data of Jou et al. [27] have also been used for the
comparison, because in this work experiments were carried out at higher
temperatures up to 413 K. In Figure 5 it can be seen that the new data and the work
of Jou et al. [27] are more in line with the relation of Jamal, so this correlation has
been used for the prediction of the solubility of N2O and CO2 in water.
0
5000
10000
15000
20000
273 293 313 333 353 373 393
T (K)
HN
2O [
kP
a m
3 k
mo
le-1
]
Jamal (2002)
Versteeg and van Swaaij (1988)
Jou (1992)
this work
Figure 5 Henry constant of N2O in water according relation of Jamal [25], Versteeg
and van Swaaij [26], experimental data from Jou et al. [27] and from this
study
CO2 solubility in aqueous MDEA 63
For the solubility data of N2O in aqueous MDEA the experimental data of several
authors have been reviewed and used in the database presented in Table 5.
Reference T [K] CMDEA [wt.%] data points
Haimour and Sandall[28] 288-308 10-20 12
Jou et al. [29] 298-398 0-40 14
Versteeg and van Swaaij [26] 293-333 4-32 50
Li and Mather [30] 303-313 30 3
Pawlak and Zarzycki [31] 293 0-100 9
Table 5 Experimental database for the solubility of N2O in aqueous MDEA
The available volumetric data must be converted from volumetric to molar units, so
the density of the solutions needs to be known. For this purpose the correlation
presented by Al-Ghawas et al. [32] was used.
With the above set of experimental data and correlations, new Huron-Vidal
interaction parameters have been determined for the CO2-MDEA binary system.
The physical solubility of CO2 in aqueous MDEA has been calculated and compared
with the results of the original model and the experimental results of Pawlak and
Zarzycki [31]. Figure 6 shows the results at 293 K; the prediction of the physical
solubility of CO2 in aqueous MDEA is much more accurate using this method.
64 Chapter 3
0
500
1000
1500
2000
2500
3000
3500
4000
0% 20% 40% 60% 80% 100%
Conc. aq. MDEA [wt.%]
H [
kP
a.m
3.k
mo
l-1]
Pawlak and Zarzycki (2002)
Solbraa (2002)
this work
Figure 6 Physical solubility of CO2 in aqueous MDEA at 293 K
All solubility data of N2O in aqueous MDEA from Table 5 have been compared with
results of the updated model. The AAD and BIAS deviation are 2.7 and 0.2 %.
3.3.3.4 CH4-MDEA
In the original model of Solbraa [7] both the molecular interaction parameter (CH4-
MDEA) and the ionic interaction parameter (CH4-MDEAH+) were determined by
regressing the model against experimental data of Addicks et al. [33] for the
quaternary reactive system (CO2-MDEA-H2O-CH4). So two parameters are obtained
from a single set of data. In this thesis a more fundamental approach is used. The
molecular interaction parameter kij for MDEA-CH4 is determined by fitting the EOS
model using a van der Waals mixing rule with experimental data for the molecular
system CH4-MDEA-H2O (Jou et al. [34]). Because the CH4-H2O and MDEA-H2O
binary interaction parameters have already been determined, the CH4-MDEA
parameter can be found by regressing against the available experimental data. Jou
et al. [34] have determined the physical solubility of CH4 in a 3 M aqueous MDEA
solution in the temperature interval of 298-403 K. A total of 44 experiments were
CO2 solubility in aqueous MDEA 65
carried out. When the experimental data of Jou et al. [34] are compared with the
model, the AAD and BIAS deviations are 10.5 and 2.2 %. In Figure 7 the results are
compared with the experimental data at 298 and 348 K.
0
20
40
60
80
100
120
140
0 0.5 1 1.5 2 2.5 3 3.5
mole fraction CH4 in liquid phase [-] *103
Pre
ssu
re [
bar]
Jou et al. @ 298 K (1998)
Model (298 K)
Jou et al. @ 348 K (1998)
Model (348 K)
Figure 7 Physical solubility of methane in aqueous 3 M MDEA
3.3.3.5 Summary
In the above sections all binary molecular interactions which are applicable in the
MDEA-H2O-CO2-CH4 system are discussed. In Table 6 the resulting interaction
parameters are presented.
66 Chapter 3
comp.i CO2 CO2 CO2 MDEA MDEA H2O
comp.j MDEA H2O CH4 H2O CH4 CH4
kij [-] 0.096 0.600
�ji [-] -0.786 0.030 0.208 0.150
�'gij [J mol-1
] 4101 30146 -9148 -1028
�'gji [J mol-1
] 2205 -18634 6095 40532
�''gij [J mol-1
K-1
] -4.01 32.53 42.35 17.40
�g''ji [J mol-1
K-1
] -5.68 -26.30 -49.93 -54.45
Table 6 Molecular interaction parameters
3.3.4 Binary ionic interaction parameters
3.3.4.1 Ionic interaction parameters in the MDEA-H2O-CO2 system
For the development of the electrolyte part of the EOS the ionic interaction
parameters Wij have to be determined. As mentioned in Section 3.2.4, only the
cation-molecule and the cation-anion interaction parameters have to be determined.
For the ternary system MDEA-CO2-H2O the interactions of the MDEAH+-ion with
MDEA, H2O, OH-, CO2, HCO3
- and CO3
2- need to be determined. Because the
concentration of OH--ions in the system is low, the MDEAH
+-OH
- binary interaction
parameter has not been fitted but estimated by the correlation given by Fürst and
Renon [9]. The remaining 5 parameters have been determined using the
experimental VLE-database of the ternary system MDEA-CO2-H2O. It must be
noted, however, that the database as used by Solbraa [7] has been modified
significantly. A detailed discussion of these changes is given by Huttenhuis et al.
[15].
The experimental database used for the determination of the MDEAH+-interaction
parameters is presented in Table 7.
CO2 solubility in aqueous MDEA 67
Ref. CMDEA
[wt.%.]
Temperature
[K]
loading
[mole CO2/mole
amine]
data
points
[-]
Lemoine et al. [35] 23.6 298 0.02-0.26 13
Austgen and
Rochelle [36]
23.4 313 0.006-0.65 14
Kuranov et al. [37] 19.2
18.8
32.1
313
313,333,373,413
313,333,373,393,
413
1.56-2.46
0.36-2.62
0.41-4.46
9
32
40
Rho et al. [38] 5
20.5
50
323
323,348,373
323,348,373
0.24-0.68
0.026-0.848
0.0087-0.385
7
32
26
Kamps et al. [16] 32.0
48.8
313
393
0.85-1.24
0.32-0.56
5
6
Huang and Ng. [39] 23
50
313,343,373,393
313,343,373,393
0.00334-1.34
0.00119-1.16
28
37
Rogers et al. [40] 23
50
313,323
313
0.000591-.1177
0.00025-0.037
20
14
Table 7 Literature references used for fitting of the ionic parameters of the MDEA-
CO2 –H2O system
The database for the determination of the MDEAH+ interaction parameters consists
of 283 data points. When the distribution of process conditions of this database is
studied the following conclusions can be drawn:
• More than 30% of the experiments were determined at conditions where the
CO2 loading is lower than 0.1 mole CO2 / mole amine;
• Most of the experimental data were determined at 313 and 373 K
(respectively 27% and 17% of the experiments);
68 Chapter 3
• Most of the experimental data were determined at 25 wt.% and 30 wt.%
MDEA (both 30% of the experiments).
The model with the new parameters (Table 8) gives AAD and BIAS deviations of
24% and 8.3%.
3.3.4.2 Ionic interactions parameters in the MDEA-H2O-CO2 –CH4 system
For the quaternary system CO2-MDEA-H2O-CH4 (with methane) four additional
interaction parameters must be determined, i.e. the MDEA-CH4 (par. 3.3.3.4), CO2-
CH4 (par. 3.3.3.1), H2O-CH4 (par. 3.3.3.1) and MDEAH+-CH4 parameters. The
molecular interaction parameters (MDEA-CH4, CO2-CH4 and H2O-CH4) have
already been determined as described in Section 3.3.3. So only one additional
parameter that of MDEAH+-CH4 has been determined by regressing the model
against experimental VLE data of Addicks et al. [33]. Addicks measured the CO2
and CH4 solubilities in aqueous MDEA. A total of 31 experimental data points have
been used for the parameter fitting. With these data the AAD and BIAS deviations
are 35% and 22% for the partial pressures of CO2 and 21.5% and –2.8% for the
total pressure. Unfortunately, the data of Addicks cannot be compared with
experimental data from other authors, because this information is unique in its kind.
In Table 8 the ionic interaction parameters are presented.
comp.i MDEAH+
MDEAH+
MDEAH+
MDEAH+
MDEAH+
MDEAH+
comp.j CO2 H2O MDEA HCO3-
CO32- CH4
Wij [m3 mol
-1] 2.48E-04 4.09E-04 1.95E-03 -1.29E-04 -3.58E-04 4.93E-04
Table 8 Ionic interaction parameters
CO2 solubility in aqueous MDEA 69
3.4 Modeling results
3.4.1 Ternary system CO2-MDEA-H2O
The CO2-MDEA-H2O model has been validated with the experimental database for
this ternary system. As described in Section 3.3.4 the AAD and BIAS are 24 and
8.3%. In Figure 8 the parity plot with the experimental database of Table 7 is
presented for different liquid loadings.
1.E-05
1.E-04
1.E-03
1.E-02
1.E-01
1.E+00
1.E+01
1.E+02
1.E+03
1.E+04
1.E-05 1.E-04 1.E-03 1.E-02 1.E-01 1.E+00 1.E+01 1.E+02 1.E+03 1.E+04
Experimental PCO2 [ kPa]
Calc
ula
ted
PC
O2 [
kP
a]
<0.001
0.001<loading<0.01
0.01<loading<0.1
0.1<loading<1
loading > 1
Figure 8 Parity plot for different liquid loadings (mole CO2/mole amine)
From this figure it can concluded that at low loadings, the partial pressure is
somewhat under-predicted by the model. The data at a CO2 partial pressure of
approximately 1 kPa, show that the predictions for the higher liquid loadings (0.1-1)
are better than the predictions at low liquid loadings (0.01-0.1). So, it seems that the
experimental data at low loadings are more scattered. In Figure 9 the experimental
70 Chapter 3
data of different authors used for the parameter regression of the present E-EOS
are compared.
1.E-05
1.E-04
1.E-03
1.E-02
1.E-01
1.E+00
1.E+01
1.E+02
1.E+03
1.E+04
1.E-05 1.E-04 1.E-03 1.E-02 1.E-01 1.E+00 1.E+01 1.E+02 1.E+03 1.E+04
Experimental PCO2 [ kPa]
Calc
ula
ted
PC
O2 [
kP
a]
Rogers et al.(1998)
Austgen and Rochelle (1991)
Huang and Ng (1998)
Rho et al. (1997)
Lemoine et al. (2000)
Kamps et al. (2001)
Kuranov et al. (1996)
Figure 9 Parity plot for different authors
In Table 9 the results of this analysis are presented together with the effect of
temperature and MDEA concentration.
CO2 solubility in aqueous MDEA 71
<0.001
(6)
0.001-0.01
(30)
0.01-0.1
(61)
0.1-1
(153)
>1
(33)
Liquid loading
[mole CO2/mole
amine] 28 28 32 38 17 28 1 22 1 11
298-313
(100)
323-333
(49)
343-353
(48)
373-393
(86) Temperature [K]
9 25 3 19 9 19 10 27
5
(21)
20-24
(135)
32
(5)
47-50
(122) CMDEA
[wt.%] 19 22 -1 17 27 27 16 31
Lemoine [35]
(13)
Austgen[36]
(14)
Rho [38]
(19)
Huang [39]
(65)
9 17 0 28 7 19 12 27
Rogers [40]
(34)
Kamps [16]
(14)
Kuranov [37]
(64)
Author
17 43 23 25 0 20
Table 9 BIAS (left column) and AAD deviation (right column) (%) for the
experimental data points as function of liquid loading, temperature, MDEA
concentration and author; number of experimental data points is given
between brackets
From this table it can be concluded that model predictions are good when the liquid
loading is above 0.1 mole CO2/mole amine, because the BIAS-deviation in this area
is only +1%. For low loadings (<0.1 mole/mole) the model always under-predicts the
CO2 partial pressure; the BIAS deviation in this area is more than +20 % and even
more than +30 % for liquid loadings below 0.01 mole/mole. There is no clear
relation between temperature and model predictions The BIAS and AAD deviations
72 Chapter 3
do not change systematically with temperature. The model predictions for the
MDEA concentration between 20-24 % are very good (BIAS = -1%). However, at
lower and higher MDEA concentrations the match between model results and
experimental data is worse. When looking to the influence of different author data
on the model predictions it can be concluded that the matches with experimental
data of Austgen et al. [36] and Kuranov et al. [37] are rather good with respect to
BIAS deviation. It must be noted, however, that Kuranov did not measure solubility
data at low liquid loadings; only high loading data were measured.
As can be concluded from Table 9, Figure 8 and Figure 9, the electrolyte equation
of state model used in this thesis gives an under-prediction of the partial pressure of
CO2, i.e. an over-prediction of the gas solubility in the low loading area. This
observation was also reported by F�rst and Planche [6], Austgen and Rochelle [36]
and Weiland et al. [41]. It must be noted that the models used by these authors
were different, so it is not clear at this state what causes these under-predictions.
The spread in the experimentally determined solubilities is much higher at low
loadings (<0.1), compared to those at high liquid loadings. Apparently the
experimental accuracy in this loading range is insufficient. To take this inaccuracy
into account in the E-EOS used here, these data were omitted from the database.
New ionic interaction parameters Wij were determined with the reduced database.
From an analysis of the results it is concluded that on average the model is not
improved significantly. There is still a large under-prediction of the CO2 partial
pressure. Therefore, the model with the ionic parameters determined with the whole
database as presented in Table 7 has been used for further study. It can also be
concluded that at lower liquid loadings a need exists for better and more reliable
experimental data.
As mentioned before one of the major advantages of the E-EOS compared to
simpler models, is that the distribution of the different species present in the liquid
can be calculated more accurately. Therefore the speciation calculated by the
CO2 solubility in aqueous MDEA 73
present model has been compared with experimentally determined speciation
carried out by Poplsteinova et al. [24]. Poplsteinova et al. measured the molecular
and ionic concentrations at equilibrium conditions for the absorption of CO2 in
different amine solutions with a NMR technique. In Figure 10 experimental data of
Poplsteinova et al. [24] are compared with the E-EOS model results.
1.0E-03
1.0E-02
1.0E-01
0 0.2 0.4 0.6 0.8 1Liquid loading [mole CO2 / mole amine]
Mo
le f
racti
on
in
liq
uid
ph
ase[-
]
MDEA MDEA
MDEAH+ MDEAH+
Figure 10 Speciation of MDEA species in 23 wt.% MDEA at 293 K calculated by the
E-EOS (lines) compared with experimental values of Poplsteinova et al.
[24] (points)
74 Chapter 3
1.0E-06
1.0E-05
1.0E-04
1.0E-03
1.0E-02
1.0E-01
0 0.2 0.4 0.6 0.8 1Liquid loading [mole CO2 / mole amine]
Mo
le f
racti
on
in
liq
uid
ph
ase[-
]
HCO3- HCO3-CO3-- CO3--CO2 CO2
Figure 11 Speciation of CO2 species in 23 wt.% MDEA at 293 K calculated by the
E-EOS (lines) compared with experimental values of Poplsteinova et al.
[24] (points)
From Figure 10 and Figure 11 it can be concluded that the speciation calculations of
the present model are well in line with the experimental data of Poplsteinova et al.
[24]. At higher liquid loadings (>0.8 mole/mole), a small over-prediction of MDEAH+
(Figure 10) and HCO3- and an under-prediction of CO3
2- (Figure 11) are seen;
however the deviations are small.
In Figure 12 and Figure 13 the activity coefficients as calculated by the E-EOS are
presented for the various species at different liquid loadings. From these figures it
can be seen that the activity of MDEAH+ (Figure 12) decreases and the activity of
HCO3- (Figure 13) increases with increasing CO2 liquid loading. The change in
activity coefficient for the other species is small. However, it must be remembered
that for all species, excluding CO2, the activity coefficients deviate substantially from
unity. It has been proven that the reaction constant based on concentrations is not a
true constant because it depends on the other non-reactive species present in the
CO2 solubility in aqueous MDEA 75
liquid phase. However when the reaction rate constant is based on activities instead
of concentrations a “true” constant can be derived and all non-idealities of the
system are incorporated in the activities of the reactive component. For example,
the influence of the counter-ion (Li, Na and K) on the reaction between the
hydroxide ion and carbon dioxide has been studied experimentally by Haubrock et
al. [42].
0
0.2
0.4
0.6
0.8
1
1.2
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid Loading [mole CO2 / mole amine]
Acti
vit
y c
oeff
icie
nt
[-]
MDEA
MDEAH+
Figure 12 Activity coefficient of MDEA species in 23 wt.% MDEA at 293 K
calculated by the E-EOS
76 Chapter 3
0
0.2
0.4
0.6
0.8
1
1.2
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid Loading [mole CO2 / mole amine]
Acti
vit
y c
oeff
icie
nt
[-]
CO2 HCO3-
CO3-- OH-
Figure 13 Activity coefficient of CO2 species in 23 wt.% MDEA at 293 K calculated
by the E-EOS model
3.4.2 Quaternary system CO2-MDEA-H2O-CH4
The system CO2-MDEA-H2O-CH4 has been validated with the experimental data of
Addicks et al. [33] and the experimental data determined as presented by
Huttenhuis et al. [15]. Results are given in Table 10.
Reference
Number
of
points
BIAS
[%]
AAD
[%]
Addicks et al. [33] 31 22 35
Appendix A [15] 51 16 30
Table 10: Model results for system CO2-MDEA-H2O-CH4
Table 10 shows that the E-EOS under-predicts the CO2 partial pressure for both
authors (BIAS > 0). In Figure 14 and Figure 15 the results of the E-EOS are
compared with the experimental data for two different amine concentrations (35
CO2 solubility in aqueous MDEA 77
wt.% and 50 wt.%). As it can be seen the prediction for the higher (50 wt.%) MDEA
concentration (BIAS = +25.2%) is poorer than the predictions for 35 wt.% MDEA
(BIAS = +5.5 %). This was also seen for the solubility data of the ternary system
(CO2-MDEA-H2O).
As can be seen from Table 9 the model predictions with MDEA concentrations of
20-24 wt.% (BIAS = -1%) are much better than the predictions for 47-50 wt.% (BIAS
= 16%). A possible explanation for this different behavior is that the CO2-N2O
analogy used for the determination of the Huron-Vidal parameters of the CO2-
MDEA system may not be applicable to the higher MDEA concentrations.
The influence of methane on the solubility of CO2 in the liquid is predicted correctly.
As can be seen from both the model and from the experiments, the CO2 solubility
decreases with increasing partial pressure of methane. Other thermodynamic
models like Kent-Eisenberg [2], Debye-Hückel [43] and NRTL [44] model do not
show this effect of an inert gas and / or system pressure on the acid gas solubility.
0.01
0.10
1.00
10.00
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35
Liquid loading [mole CO2 / mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
6.9 bar; Huttenhuis et al. (2007)
6.9 bar (model)
34.5 bar; Huttenhuis et al. (2007)
34.5 bar (model)
69 bar ; Huttenhuis et al. (2007)
69 bar (model)
Figure 14 Solubility of CO2 in 35 wt.% MDEA at 283 K
78 Chapter 3
0.10
1.00
10.00
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 0.45
Liquid loading [mole CO2 / mole amine]
CO
2 p
art
ial p
res
su
re [
kP
a]
6.9 bar; Huttenhuis et al. (2007)
6.9 bar (model)
34.5 bar; Huttenhuis et al. (2007)
34.5 bar (model)
69 bar; Huttenhuis et al. (2007)
69 bar (model)
Figure 15 Solubility of CO2 in 50 wt.% MDEA at 283 K
In Figure 16 the partial pressure, fugacity and fugacity coefficient of CO2 are
presented as function of the partial pressure of methane. From this graph it appears
that the CO2 partial pressure is increasing (which is equivalent to decreasing CO2
solubility) with the partial pressure of methane at constant CO2 liquid loadings.
However, the CO2 fugacity, remains fairly constant at the different methane partial
pressures.
CO2 solubility in aqueous MDEA 79
0
0.4
0.8
1.2
1.6
2
0 10 20 30 40 50 60 70 80
Partial pressure methane [bar]
CO
2 p
art
ial p
ressu
re / f
ug
acit
y [
kP
a]
0
0.4
0.8
1.2
1.6
2
CO
2 f
ug
acit
y c
oeff
icie
nt
[-]
CO2 partial pressure
CO2 fugacity
CO2 fugacity coefficient
Figure 16 Partial pressure, fugacity and fugacity coefficient of CO2 in 35 wt.%
MDEA at 298 K at a liquid loading of 0.1 mole CO2 / mole amine
From Figure 16 it can be concluded that the decreasing solubility of CO2 at
conditions with higher partial pressures of methane can be attributed to a
decreasing fugacity coefficient of CO2.
3.5 Conclusions
In the present study an electrolyte equation of state developed by Solbraa [7] has
been reviewed, optimized and validated with experimental data for the system
MDEA-H2O-CO2-CH4. With this model excellent results have been obtained and a
great deal of information can be derived. It has been proven (experimentally and by
the model) that the system pressure and/or partial pressure of methane have a
significant effect on the solubility of CO2 in aqueous MDEA solutions. A decrease in
CO2 solubility has been observed when the partial pressure of methane is
80 Chapter 3
increased. As the partial pressure CO2 increases with the methane partial pressure,
the CO2 fugacity becomes less dependent of the methane partial pressure. So
based on fugacities, it can be concluded that the CO2 solubility seems only slightly
dependent of methane partial pressure. At the moment it is not clear whether this
decrease in CO2 solubility is caused by the increase in pressure of the system or by
the additional methane. Model predictions are mostly in line with experimental data.
At low CO2 liquid loadings the predicted CO2 partial pressure is lower than the
experimental partial pressure. This conclusion is in line with most other authors. At
lower MDEA concentrations (<30 wt.%) model predictions are better than at high
MDEA concentrations. This phenomena may be caused by the fact the CO2-N2O
analogy used in this chapter is not applicable in more concentrated amine solutions.
List of symbols
A Helmholtz energy [J]
A Attractive term in equation of state [J.m3.mol
-1]
AAD Absolute Average Deviation [%]
B Repulsive term in equation of state [m3.mol
-1]
BIAS Mean BIAS Deviation [%]
D Coefficients for dielectric constant
D dielectric constant [-]
DEA Diethanolamine [-]
E Electron charge (1.60219*10-19
) [C]
g Interaction parameter in Huron-Vidal
mixing rule
[J.m-3
]
H Henry coefficient [kPa.m3.kmole
-1]
K Chemical equilibrium constant [-]
K Binary (molecular) interaction parameter [-]
MDEA N-methyldiethanolamine [-]
N Mole number [mole]
CO2 solubility in aqueous MDEA 81
N Avogadro’s constant (6.02205*1023
) [mole-1
]
NMR Nuclear Magnetic Resonance
P (partial) Pressure [Pa]
p1 ,p2, p3 Polarity parameters [-]
R Gas constant [J.mole-1
.K-1
]
T Temperature [K]
V Molar volume [m3.mole
-1]
W Binary ionic interaction parameter [m3.mol
-1]
X Liquid mole fraction [-]
Z Charge [-]
Greek symbols
τ Energy parameter in Huron-Vidal mixing
rule
[-]
� Binary non-randomness parameter in
Huron-Vidal mixing rule
[-]
� Correction factor for attraction
parameter ASR
[-]
�LR Long range parameter in ionic
interaction term
[m]
Shielding parameter [m-1
]
� Activity coefficient [-]
�0 Vacuum electric permittivity [C2.J
-1.m
-1]
�3 Packing factor [-]
� Ionic/molecular diameter [m]
� Accentric factor [-]
82 Chapter 3
Sub/super-scripts
∞ Infinite dilution
a Anion
aq. Aqueous
c Cation
C Critical
calc Calculated by model
exp Experiments
i,j Index
L Liquid
m Molecular
mix Mixture
R Reduced / residual
S Solvent
V Vapor
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84 Chapter 3
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composition determination in CO2-H2O-alkanolamine systems: An NMR
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monoxide in alkanolamine systems, Ph.D thesis, University of British
Columbia (2002).
CO2 solubility in aqueous MDEA 85
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(CO2, N20) in Aqueous Alkanolamine Solutions, J. Chem. Eng. Data, 33
(1988) 29-34.
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225-239.
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methyldiethanolamine, Chem. Eng. Sci., 39 (1984) 1791-1796.
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Chemical Thermodynamics (1986) Lisbon.
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mixed solvents, Fluid Phase Eq., 96 (1994) 119-142.
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water + Methyldiethanolamine and ethanol + Methyldiethanolamine
solutions, J. Chem. Eng. Data, 47 (2002) 1506-1509.
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Physicochemical Properties Important for Carbon Dioxide Absorption in
Aqueous Methyldiethanolamine, J. Chem. Eng. Data, 34 (1989) 385-391.
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Data., 43 (1998) 781-784.
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pressure of CO2 and H2S over aqueous methyldiethanolamine solutions,
Fluid Phase Eq., 172 (2000) 261-277.
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for aqueous acid gas-alkanolamine systems. 2. representation of H2S and
86 Chapter 3
CO2 solubility in aqueous MDEA and CO2 solubility in aqueous mixtures of
MDEA with MEA or DEA, Ind. Eng. Chem. Res., 30 (1991) 543-555.
[37] G. Kuranov, B. Rumpf, N.A. Smirnova, G. Maurer, Solubility of single gases
carbon dioxide and hydrogen sulfide in aqueous solutions of N-
methyldiethanolamine in the Temperature Range 313-413 K at Pressures
up to 5 MPa, Ind. Eng. Chem. Res., 35 (1996) 1959-1966.
[38] S.-W. Rho, K-P, Yoo, J.S. Lee, S.C. Nam, J.E. Son, B-M. Min, Solubility of
CO2 in aqueous methyldiethanolamine solutions, J. Chem. Data, 42 (1997)
1161-1164.
[39] S.H. Huang H.-J.Ng, Solubility of H2S and CO2 in alkanolamines, GPA
Research Report RR-155 (1998).
[40] W.J. Rogers, J.A. Bullin, R.R. Davidson, FTIR measurements of acid-gas-
methyldiethanolamine systems, AIChE J., 44 (1998), 2423-2430.
[41] R.H. Weiland, T. Chakravarty, A.E. Mather, solubility of carbon dioxide and
hydrogen sulfide in aqueous alkanolamines, Ind. Eng. Chem. Res., 32
(1993) 1419-1430.
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in kinetic expressions: A more fundamental approach to represent the
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62 (2007) 5753-5769.
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functions for liquid mixtures, AIChE J., 14 (1968) 135.
87
Chapter 4
Solubility of Hydrogen Sulfide in
Aqueous N-methyldiethanolamine
Abstract
In this chapter the electrolyte equation of state as developed previously for the
system MDEA-H2O-CO2-CH4 (P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F.
Versteeg, Fluid Phase Eq., 264 (2008) 99-112) is further developed for the system
MDEA-H2O-H2S-CH4. With this thermodynamic model the solubility of hydrogen
sulfide and the speciation in aqueous solutions of N-methyldiethanolamine can be
described quantitatively. The model results are compared with experimental H2S
solubility data in aqueous MDEA in absence and in presence of methane. The
application of an equation of state to these acid gas – amine systems is a new
development in the literature. These systems are difficult to describe because both
molecular and ionic species are present in the liquid. Schwarzentruber’s
modification of the Redlich-Kwong-Soave EOS with a Huron-Vidal mixing rule is
used as molecular part of the equation of state and ionic interactions terms are
88 Chapter 4
added to account for non-idealities caused by ionic interactions. The newly
developed model is compared with experimental data.
4.1 Introduction
Gases like CO2 and H2S are often removed to a certain extent from natural and
industrial gas streams, for environmental or operational reasons. An absorption –
regeneration process with an aqueous amine solution is commonly used. The acid
gas stream enters at the bottom in the absorber where it is contacted counter-
currently with an aqueous amine solution. In the absorber the acid components are
absorbed in the liquid and converted to non volatile ionic species. The gas stream
leaving the top of the absorber has a low acid gas concentration. The loaded
solvent from the absorber is heated and/or depressurized and sent to a stripper
where the solvent is regenerated and returned to the absorber. Thermodynamic
data, mass transfer properties and the rate of the chemical reactions need to be
known for a robust process design. Reliable thermodynamic data are necessary to
prevent costly over-design of equipment. In this thesis a rigorous thermodynamic
model (an electrolyte equation of state) is used to predict the solubility of H2S in an
aqueous MDEA solution at elevated methane pressure. In general the acid gas
solubility is determined in absence of high partial pressures of inert components like
nitrogen or hydrocarbons. However, in absorbers in the gas industry often high
methane pressures are encountered, so it is important to study the influence of
hydrocarbons on the acid gas solubility. The thermodynamic model developed in
this study has been validated with experimental data for the MDEA-H2O-H2S-CH4
system as presented by Huttenhuis et al. [5].
H2S solubility in aqueous MDEA 89
1 2
1 2 3 4 5
R R R R R R
RF SR SR LR BORN
A A A A A A
RT RT RT RT RT RT
� � � � � � � � � � � �= + + + +� � � � � � � � � � � �
� � � � � � � � � � � �
4.2 The electrolyte equation of state
An equation of state uses the same equations for both the vapor and liquid. This
also applies to the electrolyte equation of state (E-EOS). In the present study
Schwarzentruber’s [1] modification of the Redlich-Kwong-Soave EOS with a Huron-
Vidal [2] mixing rule is used. Additional interactions are added to this equation of
state to allow for ions in the liquid as originally proposed by Fürst and Renon [3]. A
major advantage of this approach is that complex multi-component systems can be
described quantitatively by studying less complex systems containing a smaller
number of components. The system CO2-MDEA-H2O-CH4 is described with an E-
EOS by Huttenhuis et al. [6]: in this chapter the system H2S-MDEA-H2O-CH4 is
dealt with. The parameters of the system MDEA-H2O-CH4 are already known from
the system CO2-MDEA-H2O-CH4 and these are used in the new model. Only
additional pure component data and interaction parameters due to the presence of
H2S and its related ionic species are required.
The electrolyte equation of state used in this study contains the following terms:
Equation 1
The first two terms describe the molecular equation of state – here the Redlich-
Kwong-Soave EOS as modified by Schwarzentruber (ScRK-EOS) [1]. To account
for interactions between molecules the Huron-Vidal mixing rule is used, because
this mixing rule can also be used for highly non-ideal (polar) molecular systems,
such as MDEA-H2O. In this mixing rule 5 interaction parameters are required for
each binary molecular system. Another advantage of this Huron-Vidal mixing rule is
that it can easily be converted to the van der Waals mixing rule using only one
interaction parameter per binary pair. The other terms in the Helmholtz expression
are to allow for interactions with the ions in the system. For a detailed description of
the E-EOS used in this thesis reference is made to Huttenhuis et al [6].
90 Chapter 4
4.3 Model development
4.3.1 Former work
As described above the system MDEA-H2O-CH4 which is part of the H2S-MDEA-
H2O-CH4 system was already described quantitatively in Chapter 3. Only additional
pure component and interaction parameters for H2S and the related ionic species
are required.
The following additional information is required to account for the presence of H2S
in the system:
• Pure component parameters of H2S, HS- and S
2-;
• Molecular interactions of the binary systems: H2S-MDEA, H2S-H2O and
H2S-CH4;
• Ionic interaction parameters for: H2S-MDEAH+, HS
--MDEAH
+, S
2--MDEAH
+.
In the scheme shown in Figure 1 an overview of the involved pure and binary
parameters is presented for the H2S-MDEA-H2O-CH4 system.
H2S solubility in aqueous MDEA 91
��� ���� ��� ��
������������������
��������������
������ �������� ��
��������
��������
������� ��������� ��
����� ������� ��
������������� �������
���� � ���������������������������������������
�����������������������������
��������������������������������
Figure 1 Overview of the interactions involved in the E-EOS model for the system
H2S-MDEA-H2O-CH4
4.3.2 Chemical reactions
When hydrogen sulfide absorbs in the liquid several acid-base reactions take place
and ionic species are formed. For the H2S-MDEA-H2O-CH4 system the following
reactions take place:
water dissociation: 1
2 32K
H O H O OH+ −
←⎯→ + (K1)
bisulfide formation: 2
2 2 3
KH O H S HS H O
− ++ ←⎯→ + (K2)
Sulfide formation: 3 2
2 3
KH O HS S H O
− − ++ ←⎯→ + (K3)
MDEA protonation 4
2 3
KH O MDEAH MDEA H O
+ ++ ←⎯→ + (K4)
92 Chapter 4
ln lnx
BK A C T
T= + +
The relation between the equilibrium constant Kx and temperature is:
Equation 2
The parameters for the equilibrium constants are given in Table 1.
KX A B C T [K] Reference
K1 132.899 -13445.9 -22.4773 273-498 Austgen [8]
K2 214.582 -12995.4 -33.5471 273-423 Austgen [8]
K3 -32.0 -3338.0 0.0 287-343 Austgen [8]
K4 -77.262 -1116.5 10.06 278-423 Huttenhuis et al. [5]
Table 1 Parameters to calculate the equilibrium constants of system H2S-MDEA-
H2O
The K1 and K4 relations are the same as used by Huttenhuis et al. [6] for the system
MDEA-H2O-CO2. In this thesis all chemical equilibrium constants are defined in the
mole fraction scale with infinite dilution in water as reference state for all species.
The concentration of H3O+-ions is neglected, because the mole fraction of this
component is very low. The thermodynamic model is able to calculate the mole
fraction in both the gas and liquid of the following species: H2O, OH-, H2S, HS
-, S
2-,
MDEA, MDEAH+ and CH4.
4.3.3 Pure component model
In the MDEA-H2O-H2S-CH4 system the following species are present: MDEA,
MDEAH+, H2O, H3O
+, OH
-, H2S
- HS
-, S
2- and CH4. The pure component parameters
of these components are the same as used by Huttenhuis et al. [6] except the
following values, which are taken from Vallée et al. [4]:
H2S solubility in aqueous MDEA 93
H2S HS- S
2-
M [gram.mole-1
] 34.08 33.08 32.08
TC [K] 100.05
PC [bar] 89.37
� [-] 0.1
p1 0.01857
p2 0
p3 -2.078
� [10-10
m] 3.62 3.6 3.5
d(0)
2
d(1)
0
d(2)
0
d(3)
0
Table 2 Pure component parameters
4.3.4 Binary molecular interaction parameters
4.3.4.1 Overview
For the determination of the binary molecular interaction parameters, the same
approach as presented by Huttenhuis et al. [6] is followed. Before simulating the
quaternary system H2S-MDEA-H2O-CH4, the following binary systems have to be
studied and optimized:
• H2S-H2O: For this system the binary interaction data were determined from
the three following sources: Selleck et al. [9], Lee and Mather [10] and
Clarke and Glew [11] ;
• H2S-MDEA: For this molecular binary system no experimental data are
available, because it is difficult to measure the physical solubility of H2S in
94 Chapter 4
pure MDEA. This is because trace amounts of water which are always
present in the MDEA increase the solubility significantly. Therefore the N2O
analogy was used as frequently applied for CO2;
• CH4-H2S: The van der Waals equation was used with an interaction
parameter kij = 0.08 [19];
• CH4-MDEA, H2O-MDEA, CH4-H2O: For these binary molecular systems the
same interaction parameters as used by Huttenhuis et al. [6] were
incorporated in the model.
4.3.4.2 H2S-H2O
From an evaluation it was concluded that the experimental data of the following
sources were consistent: Selleck et al. [9], Lee and Mather [10] and Clarke and
Glew [11]. Lee and Mather [10] measured the total system pressure at a specified
temperature and H2S liquid concentration. Selleck et al. [9] and Clarke and Glew
[11] measured both the system pressure and the H2S vapor concentration. In the
paper of Selleck et al. [9] also extrapolated data and experimental data with two
liquid phases are presented, however these are not used in this chapter, because
our E-EOS cannot deal with two liquid phases at this stage. The experimental data
(both system pressure and vapor concentration) are used to determine the binary
Huron-Vidal parameters of the H2S-H2O system. The experimental conditions of
these literature sources and the comparison with the EOS are presented in Table 3.
H2S solubility in aqueous MDEA 95
Model Results
P [bar] T [K] Data P [bar] yH2S [-]
BIAS
[%]
AAD
[%]
BIAS
[%]
AAD
[%]
Clarke and Glew [11] 0.5-0.95 273-323 36 -4.0 4.4 -0.04 0.15
Lee and Mather [10] 1.5-66.7 283-453 325 0.64 3.0 n.a. n.a.
Selleck et al. [9] 6.9-121 311-444 26 3.2 4.8 -0.11 0.40
Total 0.5-121 273-453 387 0.36 3.2 -0.07 0.25
Table 3 Experimental conditions and model results for the H2S-H2O system
The AAD and BIAS are defined as:
,exp , ,exp ,
1 1,exp ,exp
1 1100% 100%
n n
acidgas acidgas calc acidgas acidgas calc
i iacidgas acidgas
P P P PAAD BIAS
n P n P= =
− −= ⋅ = ⋅� �
From Table 3 it can be concluded that the model results are well in line with the
three literature sources. In Figure 2 the experimental data of Lee and Mather [10]
are compared with the model results. Figure 3 compares the experimental data of
Selleck et al [9] and Clarke and Glew [11] with the model. The data of Clarke and
Glew are measured over small temperature intervals (of 5 K), so not all data are
shown in the graph. However, for the model regression all experimental data have
been used.
96 Chapter 4
1
10
100
0.0001 0.001 0.01 0.1xH2S [-]
Pto
tal [b
ara
]
283 K 293 K
303 K 323 K
344 K 363 K
423 K 453 K
Figure 2 Total pressure against the H2S liquid concentration for the H2S-H2O
system; model results compared with experimental data of Lee and
Mather [10]
H2S solubility in aqueous MDEA 97
0.1
1
10
100
0.0001 0.001 0.01 0.1
xH2S [-]
Pto
tal [b
ara
] Selleck 311 K
Selleck 344 K
Selleck 378 K
Selleck 411 K
Selleck 444 K
Clarke 273 K
Clarke 288 K
Clarke 313 K
Figure 3 Total pressure against the H2S liquid concentration for the H2S-H2O
system; model results compared with experimental data of Selleck et al.
[9] and Clarke and Glew [11]
4.3.4.3 H2S-MDEA
For this molecular binary system no direct experimental data are available, because
it is difficult to measure the physical solubility of H2S in MDEA. This is because
trace amounts of water present in MDEA will cause chemical reactions and the
formation of ionic species. Therefore the same approach as used by Huttenhuis et
al. [6]. The physical solubility of H2S in aqueous MDEA is determined from the N2O
analogy as is frequently used to determine the physical solubility of CO2 in reactive
solvents. According to this H2S-N2O analogy the physical solubility of H2S in
aqueous MDEA can be calculated in the following manner:
98 Chapter 4
2
2 2
2
,
, . , .
,
H S water
H S aq MDEA N O aq MDEA
N O water
HH H
H= ⋅
Equation 3
The experimental data for the solubility of N2O in water and N2O in aqueous MDEA
are taken from Huttenhuis et al. [6] and the solubility of H2S in water is taken from
the data of Clarke and Glew [11], Lee and Mather [10] and Selleck et al. [9] for the
H2S-H2O system (refer to Section 4.3.4.2)
The physical solubility of H2S in aqueous MDEA can be calculated, when the
interaction parameters of the following binary molecular systems are known: MDEA-
H2O, H2S-H2O and H2S-MDEA. So in the present case the unknown binary
interaction parameters of the H2S-MDEA system can be calculated when the binary
molecular interactions of H2S-H2O (refer to Section 4.3.4.2) and MDEA-H2O
(Huttenhuis et al. [6]) and the physical solubility of H2S in aqueous MDEA (see
above) are known. The physical solubility of N2O in water is based on the relation
developed by Jamal [12]. The physical solubility of N2O in aqueous MDEA is based
on experimental data produced by the following authors:
• Versteeg and van Swaaij [13];
• Haimour and Sandall [14];
• Jou et al. [15];
• Li and Mather [16];
• Pawlak and Zarzycki [17].
In the work carried out by Rinker and Sandall [18] the physical solubility of H2S was
determined by neutralizing the aqueous MDEA solvent with HCl. In Figure 4 the
calculated physical solubility of H2S using the N2O analogy (based on experimental
data of Versteeg and van Swaaij, Haimour and Sandall and Jou et al.) is compared
with the experimental data in neutralized aqueous MDEA as reported by Rinker and
Sandall [18].
H2S solubility in aqueous MDEA 99
0
500
1000
1500
2000
2500
273 283 293 303 313 323 333 343 353 363 373
Temperature [K]
HH
2S
[kP
a.m
3.k
mo
le-1
]
Versteeg and van Swaaij (1988)
Haimour and Sandall (1984)
Jou et al. (1986)
Rinker & Sandall (2000)
Figure 4 Physical solubility of H2S in aqueous 20 wt.% MDEA as function of
temperature
From Figure 4 it can be concluded that the physical solubility of H2S in aqueous
MDEA using the N2O analogy ([13], [14] and [15]) is very well in line with the
physical solubility determined in neutralised aqueous MDEA [18].
After the new binary interaction parameters for the H2S-MDEA system were
calculated from the experimental data, the calculated physical solubility of H2S in
aqueous MDEA was compared with the physical solubility calculated by the updated
EOS; the results were good (BIAS of 0.61 % and AAD of 8.8%).
100 Chapter 4
4.3.4.4 H2S-CH4
During the model simulations it was found that the calculated H2S solubility was not
sensitive to the value of the molecular interaction parameter of the H2S-CH4 binary
system. Therefore it was decided to use a value of 0.08 for the binary interaction
parameter kij of the van der Waal mixing rule, based on a binary interaction
parameter kij for the binary system H2S-propane [19].
4.3.4.5 Summary
In this chapter all molecular interaction parameters for describing the system H2S-
MDEA-H2O-CH4 have been determined. These parameters are shown in Table 4:
comp.i H2S H2S H2S MDEA MDEA H2O
comp.j MDEA H2O CH4 H2O CH4 CH4
kij [-] - - 0.08 - 0.600 -
�ij [-] -0.907 0.104 - 0.208 - 0.150
�’gij [Jmol-1
] 5567 26082 - -9148 - -1028
�’gji [Jmol-1
] 2928 -2148 - 6095 - 40532
�’gij [Jmol-1
K-1
] -2.44 -18.45 - 42.35 - 17.40
�’gij [Jmol-1
K-1
] 15.11 5.76 - -49.93 - -54.45
reference This
work
This
work
This
work
Huttenhuis
et al. [6]
Huttenhuis
et al. [6]
Huttenhuis
et al. [6]
Table 4 Binary molecular interaction parameters
The binary molecular interaction parameters MDEA-H2O, MDEA-CH4 and H2O-CH4
were derived from systems containing no acid gas (CO2 or H2S), so the same
values as used by Huttenhuis et al. [6] were used for these interaction parameters.
H2S solubility in aqueous MDEA 101
4.3.5 Binary ionic interaction parameters
4.3.5.1 Ionic interaction parameters in MDEA-H2S-H2O system
Following the work of Fürst and Renon [3], only the cation-anion and cation-
molecular ionic interaction parameters are regressed in the model. The cation-
cation, anion-anion and anion-molecular interactions are neglected. To describe the
ternary system H2S-MDEA-H2O, the following ionic interaction parameters need to
be determined:
• MDEAH+
- MDEA;
• MDEAH+
- H2O;
• MDEAH+
- H2S;
• MDEAH+
- HS-;
• MDEAH+
- S2-
.
The first two interaction parameters (MDEAH+-MDEA and MDEAH
+-H2O) are
independent of the acid gas type. These interaction parameters have already been
regressed by Huttenhuis et al. [6] for the CO2-MDEA-H2O system. However, the
other ionic interaction parameters, which are H2S specific, have to be derived from
experimentally H2S solubility data presented in literature. Before using the published
experimental data of various research groups, a consistency check was carried out
on the applicability of the data. The MDEA-H2S-H2O solubility data of the following
authors were reviewed with mutual and internal consistency tests: Maddox et al.
[20], Lemoine at al. [21], Huang and Ng [22], Kamps et al. [23], Kuranov et al. [24],
MacGregor and Mather [25], Rogers and Bullin [26], Sidi-Boumedine et al. [27], Jou
et al. [28] and [29], Li and Shen [30].
An overview of the experimental data used for model regression is presented in
Table 5.
102 Chapter 4
Ref. CMDEA
[wt.%]
Temperature
[K]
loading
[mole H2S/mole
amine]
Data points
[-]
Lemoine at al.
[21]
11.8
23.6
298
313
0.01-0.26
0.015-0.15
16
13
Maddox et al.
[20]
11.8
20
298
311, 339, 389
0.64-2.17
0.18-1.59
19
30
Huang and Ng
[22]
23.1
50
313, 373, 393
313, 343, 373,
393
0.003-0.20
0.003-1.74
8
33
Kamps et al. [23] 48.8 313, 353, 393 0.15-1.43 26
Kuranov et al.
[24]
18.7
32.2
313, 333, 373,
393, 413
313, 333, 373,
393, 413
0.50-1.93
0.48-1.63
35
36
MacGregor and
Mather [25]
20.9 313 0.13-1.73 27
Rogers and Bullin
[26]
23
50
313
313
0.013-0.31
0.0022-0.093
12
10
Sidi-Boumedine
et al. [27]
46.8 313, 373 0.039-1.12 26
Table 5 Literature references used for the fitting of the ionic parameters of the
H2S-MDEA-H2O system; total 291 data points
The data of Jou et al. [28] and [29] and Li et al. [30] were not included in the
database which was used to determine the ionic interaction parameters for the
following reasons:
• When the presented experimental data of Jou et al. [28] at 313 K were
compared for self-consistency, it was concluded that there was almost no
difference in H2S solubility between 35 wt.% and 49 wt.% aqueous MDEA.
This seems questionable, because at fixed loading and temperature, the
H2S solubility in aqueous MDEA 103
acid gas partial pressure increases with the MDEA concentration (refer to
Chunxi and Fürst [31]);
• Data of Jou et al. [29] in 50 wt.% MDEA were not consistent at loadings
below 0.05. The trend of a log-log graph of the liquid loading versus H2S
partial pressure at low loadings should be almost linear and this was not the
case. There was also a mutual inconsistency when Jou’s data were
compared with data of Lemoine et al. [21], Huang and Ng [22] and Rogers
and Bullin [26]. For more details reference is made to Huttenhuis et al. [5];
• Data of Li et al. [30] at higher temperature are highly non-linear at elevated
temperatures as can be seen in Figure 5. At low loadings (< 0.3), a linear
relation between the logarithm of the partial pressure and the gas loading
exists for acid gas – aqueous alkanolamine systems (refer to Chunxi and
Fürst [31]).
1
10
100
1000
0.01 0.1 1
Liquid loading [mole CO2 / mole amine]
PH
2S [
kP
a]
313 K
333 K
353 K
373 K
Figure 5 Solubility of H2S in 2.57 M aqueous MDEA at different temperatures (Li et
al. [30])
104 Chapter 4
With the experimental solubility data in Table 5 all binary ionic interaction
parameters have been determined except the MDEAH+
- S2-
interaction parameter.
Because the concentration of S2-
will be low (due to the low dissociation constant of
the bisulfide ion) the influence of the MDEAH+
- S2-
ionic interaction parameter is
negligible and therefore this parameter is not regressed with the experimental
solubility data of H2S in aqueous MDEA. This ionic interaction parameter was
calculated with the correlation proposed by Chunxi and Fürst [31]. The other ionic
binary interaction parameters Wij have been determined by regressing the
electrolyte equation of state with the experimental database given in Table 5. The
values of all derived binary ionic interaction parameters are presented in Table 6.
comp.i MDEAH+ MDEAH
+ MDEAH
+ MDEAH
+ MDEAH
+
comp.j MDEA H2O H2S HS- S
2-
Wij [m3mol
-1] -1.16E-04 6.17E-05 2.58E-05 -1.46E-04 2.52E-05
Table 6 Ionic interaction parameters regressed with solubility data of H2S in
aqueous MDEA
The AAD and BIAS deviations for the H2S experiments derived from these
regressions are 19% and 3.6%. The binary interaction parameters which are not
acid gas specific (MDEAH+-MDEA and MDEAH
+-H2O) were compared with the
values of these parameters regressed by Huttenhuis et al. [6]. In that work these
interaction parameters were derived from experimental solubility data of CO2 in
aqueous MDEA; in Table 7 these regressed ionic interaction parameters are shown.
H2S solubility in aqueous MDEA 105
comp.i MDEAH+ MDEAH
+ MDEAH
+ MDEAH
+ MDEAH
+
comp.j MDEA H2O CO2 HCO3- CO3
2-
Wij [m3mol
-1] 1.95E-03 4.09E-04 2.48E-04 -1.29E-04 -3.58E-04
Table 7 Ionic interaction parameters regressed with solubility data of CO2 in
aqueous MDEA (refer to Huttenhuis et al. [6])
From Table 6 and Table 7 it can be concluded that the common interaction
parameters of the single H2S and single CO2 solubility experiments do not coincide
at all. The MDEAH+-H2O interaction parameter is an order of magnitude higher for
CO2 compared to that for H2S. The difference for the MDEAH+-MDEA parameter is
even higher; here the H2S parameter has a negative sign, while the CO2 parameter
has a positive value!
One of the aims of using the E-EOS is to obtain a unique set of model parameters.
So the differences in regressed ionic interaction parameters are unacceptable and
have to be eliminated. Therefore a different approach was used to determine the
ionic binary interaction parameters Wij. All seven interaction parameters reported in
Table 6 and Table 7 were regressed simultaneously with both the experimental
solubility data of H2S-only in aqueous MDEA and CO2–only in aqueous MDEA. So
the experimental databases of this chapter (H2S solubility) and of Chapter 3 (CO2
solubility) are used simultaneously for model regression. The same approach was
used by Chunxi and Fürst [31]. From the simultaneous regression with CO2–only
and H2S–only solubility data, the following values for the ionic binary interaction
parameters were derived (Table 8).
106 Chapter 4
comp.i MDEAH+ MDEAH
+ MDEAH
+ MDEAH
+
comp.j MDEA H2O H2S HS-
Wij [m3mol
-1] 2.31E-03 4.17E-04 4.88E-04 -1.49E-04
comp.i MDEAH+ MDEAH
+ MDEAH
+
comp.j CO2 HCO3- CO3
2-
Wij [m3mol
-1] 2.98E-04 -1.32E-04 -2.74E-04
Table 8 Ionic interaction parameters regressed with solubility data of H2S in
aqueous MDEA and CO2 in aqueous MDEA simultaneously
When the values of the ionic interaction parameters as presented in Table 8 are
compared with the values presented in Table 6 and Table 7 it can be concluded
that:
• The values of the new common (H2S and CO2) interaction parameters
(MDEAH+-MDEA and MDEAH
+-H2O) have changed substantially compared
to the values derived from the single gas H2S experiments specified in
Table 6. However, differences compared with the values derived from the
CO2–only experiments presented in Table 7 are significantly lower. The
value of the MDEAH+-MDEA interaction parameter has increased 18 %
while the MDEAH+-H2O interaction parameters has increased by only 2 %.
The values of the CO2 specific interaction parameters (MDEAH+-CO2, MDEAH
+-
HCO3-, MDEAH
+-CO3
2-) have not changed significantly due to the addition of the
H2S-only data in the regression procedure. The maximum change was seen for the
MDEAH+-CO3
2- interaction parameter which showed an increase of 23 % owing to
the change in the MDEAH+-MDEA interaction parameter. However, because of the
low concentrations of CO32-
in loaded amine solutions, the value of this parameter
will have only a minor influence on the overall results of the E-EOS. The prediction
of the E-EOS with the new ionic interaction parameters Wij specified in Table 8 were
compared with the experimental CO2–only solubility data from Huttenhuis et al. [6].
H2S solubility in aqueous MDEA 107
Similar results are obtained with the new interaction parameters. The calculated
AAD and BIAS of the experiments changed from 24 % [6] to 25 % and from 8.3 %
[6] to 8.4 % respectively.
However, the H2S specific ionic interaction parameter (MDEAH+-H2S) and the ionic
interaction parameters MDEAH+-MDEA and MDEAH
+-H2O, which are independent
of acid gas type, changed significant when the parameter regression was carried
out with solubility data of CO2 and H2S simultaneously, compared with regression of
these parameters with H2S–only solubility data. For the H2S solubility experiments,
the BIAS deviation improved from 3.6% (H2S-only) to 2.1 % (H2S and CO2
simultaneously), while the AAD deviation increased from 19% to 26%.
In Table 9 the AAD and BIAS deviations of the E-EOS calculations with the different
sets of ionic interaction parameters are given.
CO2 H2S
Table 7 Table 8 Table 6 Table 8
AAD [%] 24 25 19 26
BIAS [%] 8.3 8.4 3.6 2.1
Table 9 AAD and BIAS deviations for H2S-only and CO2–only experiments; ionic
interaction parameters based on Table 6, Table 7 and Table 8
respectively
4.3.5.2 Ionic interaction parameters in H2S-MDEA-H2O-CH4 system
Only one additional ionic interaction parameter is required when methane is added
to the H2S-MDEA-H2O system, i.e. that of MDEAH+-CH4. This parameter has been
determined in a previous study [6]. The value of this parameter has been
determined by regressing this interaction parameter with experimental solubility
data of Addicks et al. [7], who measured the solubility of CO2 in aqueous MDEA at
elevated methane partial pressure. However due to the new ionic interaction
parameters determined in this chapter as described in 4.3.5.1 the regression of this
108 Chapter 4
parameter with Addick’s experimental solubility data has been repeated. This
MDEAH+-CH4 ion interaction parameter changed marginally from 4.93E-04 to
5.77E-04.
4.3.5.3 Summary
All relevant ionic interaction parameters have been determined to characterize the
H2S-MDEA-H2O-CH4 system. It must be noted that the ionic interaction parameters
which were used to describe the system CO2-MDEA-H2O-CH4 as determined by
Huttenhuis et al. [6] were changed marginally.
4.4 Modeling results
4.4.1 Ternary system H2S-MDEA-H2O
With the derived parameters of the electrolyte equation of state, new calculations
have been carried out to compare the model with the experimental database of
Table 5. The calculated AAD and BIAS deviations between model and experimental
data are 26% and 2 %. Figure 6 shows a parity plot of the H2S solubilities for
different H2S liquid loadings.
H2S solubility in aqueous MDEA 109
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
1.0E+04
1.0E-03 1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02 1.0E+03 1.0E+04
Experimental PH2S [kPa]
Calc
ula
ted
PH
2S [
kP
a]
loading<0.01
0.01<loading<0.1
0.1<loading<1
loading>1
Figure 6 Parity plot for different H2S liquid loadings (mole H2S/mole amine)
At low loadings (< 0.1 mole H2S / mole amine) the predicted H2S partial pressures
are consistently lower than the experimental data. The same conclusion was made
by Huttenhuis et al. [6], where the CO2-MDEA-H2O system was studied. Both the
AAD and BIAS deviations decreased significantly for an H2S liquid loading above
0.1 mole H2S / mole amine. For intermediate loadings (0.1 < loading < 1) a negative
BIAS is found for low partial pressures and a positive BIAS for higher partial
pressures. The best model results were obtained for very high H2S liquid loadings
(loading > 1). In this region the calculated BIAS was zero for the 96 experimental
data points. The influence of temperature and MDEA concentration on the model
performance was also analysed, however no clear conclusion could be drawn. At
intermediate temperature (311-313 K) and intermediate MDEA concentrations (20-
24 wt.%) a negative BIAS (Pexp < Pmodel) is found, while for all other conditions BIAS
110 Chapter 4
deviations are positive (Table 10). In Figure 7 the E-EOS predictions are compared
with the experimental data of the different research groups.
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
1.0E+04
1.0E-03 1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02 1.0E+03 1.0E+04
Experimental PH2S [kPa]
Calc
ula
ted
PH
2S [
kP
a]
Lemoine et al. (2000)
Maddox et al. (1987)
Huang and Ng (1998)
Kamps et al. (2001)
Kuranov et al. (1996)
MacGregor and Mather (1991)
Rogers and Bullin (1998)
Sidi-Boumedine et al. (2004)
Figure 7 Parity plat for data of different research groups
It is clear that the model under-predicts all H2S partial pressure data at partial
pressures lower than 1 kPa (low H2S liquid loadings). Also a lot of scatter is seen in
this range (AAD > 25 %). A probable explanation for this is that the MDEA used was
contaminated with small amounts of primary and/or secondary amines. These
contaminants usually have a higher pKa and therefore reduce the observed
equilibrium partial pressures, especially at low loadings.
In the intermediate region (1 < PH2S < 1000 kPa) the experimental data of
MacGregor and Mather [25] are remarkable. The BIAS and AAD for this data set
are -60% and +60%; the H2S partial pressures are always lower than the model
H2S solubility in aqueous MDEA 111
estimations. This is not in line with the data of the other authors, which agree well
with model predictions for intermediate H2S partial pressures and show positive
BIAS deviations for low and high partial pressures. The same conclusion was
presented by Huttenhuis et al. [6] with respect to the work of Jou et al. ([28] and
[29]) who measured the solubility of CO2 in aqueous MDEA. It was concluded In
Appendix A that the solubility data of Jou et al. show CO2 partial pressures which
are significantly lower compared to the results of other authors at similar process
conditions. MacGregor and Mather [25] measured the solubility of H2S in 20.9 wt.%
MDEA at 313 K; so the influence of their data on the model predictions is the reason
that negative BIAS deviations are seen in the intermediate temperature range of
311-313 K and intermediate MDEA concentrations (20-24 wt.%). When the data of
MacGregor and Mather [25] are excluded from the AAD and BIAS calculations for
Table 8, the BIAS deviations for the temperature range of (311-313 K) and MDEA
concentration range of (20-24 wt.%) change from respectively -11% to +4 % and -
16% to -4% (respectively BIAS and AAD)! Comparing these results with those
calculated by Huttenhuis et al. [6]) for the CO2-MDEA-H2O system shows that the
accuracy of the model for H2S is similar to that for CO2. For the different data
sources, the best matching is obtained for the experimental data of Maddox et al.
[20] and Kuranov et al. [24]. However, it should be noted that for these two sources
experiments were carried out at relatively high acid gas partial pressures. These
experiments are less difficult, than experiments at low acid gas partial pressures.
112 Chapter 4
Table 10 BIAS (left column) and AAD deviation (right column) (%) for the
experimental data points as function of liquid loading, temperature,
MDEA concentration and author; number of experimental data points is
given between brackets
One of the advantages of the E-EOS model compared with less rigorous models is
that the activity coefficient and speciation of each component in the liquid can be
calculated. This speciation is important when rate based absorption models are
required to predict the mass transfer rates in gas treating equipment. Figure 8
(MDEA and MDEAH+) and Figure 9 (H2S and HS
-) show the speciation of the
species in a 35 wt.% aqueous MDEA solution at 313 K as calculated with the E-
EOS.
<0.01
(14)
0.01-0.1
(45)
0.1-1
(136)
>1
(96)
Liquid loading
[mole H2S/mole
amine] 32 34 19 34 -5 31 0 14
298-299
(35)
311-313
(121)
333-353
(41)
373-413
(94) Temperature [K]
8 27 -11 30 14 19 11 22
12
(35)
20-24
(125)
32
(36)
47-50
(95)
Concentration
MDEA
[wt.%] 8 27 -16 26 11 17 20 29
Lemoine et al.
[21]
(29)
Maddox et al.
[20]
(49)
Huang and Ng.
[22]
(41)
Kamps et
al. [23]
(26) Author
25 28 -5 17 6 29 31 31
Kuranov et al.
[24]
(71)
MacGregor
and Mather
[25]
(27)
Rogers and Bullin
[26]
(22)
Sidi-Boumedine et
al. [27]
(26) Author
4 13 -60 60 8 38 9 17
H2S solubility in aqueous MDEA 113
1.0E-06
1.0E-05
1.0E-04
1.0E-03
1.0E-02
1.0E-01
1.0E+00
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid loading [mole H2S / mole amine]
Mo
le f
racti
on
in
liq
uid
ph
ase [
-]
MDEA
MDEAH+
Figure 8 Speciation of MDEA species in 35 wt.% MDEA at 313 K calculated by the
E-EOS
114 Chapter 4
1.0E-06
1.0E-05
1.0E-04
1.0E-03
1.0E-02
1.0E-01
1.0E+00
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid loading [mole H2S / mole amine]
Mo
le f
racti
on
in
liq
uid
ph
ase [
-]
H2S
HS-
Figure 9 Speciation of H2S species in 35 wt.% MDEA at 313 K calculated by the E-
EOS
The calculated mole fractions of the S2-
-ion in the liquid phase are lower than 10-9
for all liquid loadings, so this species has been omitted in Figure 9. Because of the
low concentration of S2-
the fraction of the MDEAH+-ion is almost identical to that of
the HS--ion. In Figure 10 and Figure 11 the calculated activity coefficients are
presented for all species present in the H2S-MDEA-H2O system.
H2S solubility in aqueous MDEA 115
0
0.5
1
1.5
2
2.5
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid loading [ mole H2S / mole amine]
acti
vit
y c
oeff
icie
nt
[-]
H2O
MDEA
MDEAH+
Figure 10 Activity coefficient of MDEA species in 35 wt.% MDEA at 313 K
calculated by the E-EOS
116 Chapter 4
0
0.5
1
1.5
2
2.5
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Liquid loading [ mole H2S / mole amine]
acti
vit
y c
oeff
icie
nt
[-]
H2S
HS-
Figure 11 Activity coefficient of H2S species in 35 wt.% MDEA at 313 K calculated
by the E-EOS
From Figure 10 and Figure 11 it can be concluded that the MDEAH+ activity
coefficient decreases and the HS- activity coefficient increases as the H2S liquid
loading increases. For the other species in the liquid, the influence of the H2S liquid
loading on the activity coefficient is less pronounced. The activities of H2O and H2S
are close to unity over a wide range of liquid loadings. However, the MDEA activity
is lower than unity at low loadings but, remarkably, it increases with the loading and
at 0.9 it even becomes larger than 1. The same behavior for the activity and
speciation was seen in the system CO2-H2O-MDEA (Huttenhuis et al. [6]). The main
difference is that the concentration of S2-
in the liquid can be neglected over the
entire range of H2S liquid loadings, but for CO2, the CO32-
concentration is
significant. This is due to the difference in dissociation constants of HS- and HCO3
-.
H2S solubility in aqueous MDEA 117
The dissociation constant Ka of HS- is more than two orders of magnitude higher
than that of HCO3-.
In Figure 12 the H2S partial pressure as calculated with the E-EOS model is shown
for a 35 wt.% aqueous MDEA solution with a liquid loading of 0.5 as a function of
temperature. The same calculations have been carried out for the solubility of CO2
in aqueous MDEA with the model previously developed [6].
1
10
100
283 303 323 343 363
Temperature (K)
Pa
cid
ga
s [
kP
a]
P-CO2
P-H2S
Figure 12 Calculated partial pressure CO2 and H2S in 35 wt.% MDEA at a acid gas
liquid loading of 0.5 mole acid gas / mole amine
118 Chapter 4
From Figure 12 it can be concluded that at 313 K, H2S and CO2 solubilities are
comparable in 35 wt.% MDEA. With increasing temperature the acid gas solubility
for H2S becomes higher than for CO2. This effect can be explained by the influence
of the temperature on the acid gas dissociation constants and physical solubilities of
both acid gases in the liquid. In Figure 13 the dissociation constants (pKa’s) and the
Henry constants in water are presented as function of temperature for both H2S and
CO2.
7.5
8
8.5
9
9.5
283 293 303 313 323 333 343 353 363
Temperature (K)
pK
ac
id g
as [
-]
0
2
4
6
8
10
H [
MP
a.k
g.m
ol-1
]
pK-CO2 pK-H2S
H-CO2 H-H2S
Figure 13 Acid gas dissociation constant (based on mole fractions) for CO2 [32] and
H2S [8] and acid gas Henry constant in water [24] as function of
temperature
In Figure 13 it can be seen that over the temperature range 283-363 K, the pKa of
CO2 is lower than for H2S (i.e. CO2 is a stronger acid), meaning that more molecular
CO2 will dissociate as ionic species in water. On the other hand, the Henry constant
of CO2 in water is higher than that of H2S, i.e. the solubility of CO2 in water is lower
H2S solubility in aqueous MDEA 119
than that of H2S in water. According to the N2O analogy as mentioned in 4.3.4.3, the
acid gas solubility in water can be correlated with the physical solubility in aqueous
MDEA when the N2O solubilities in water and aqueous MDEA are known. So from
the Henry constant presented in Figure 13 it can be concluded that the physical
solubility in H2S in aqueous MDEA is substantially higher than the physical solubility
of CO2. So due to the lower acidity of H2S and the higher physical solubility in
aqueous MDEA compared to CO2, it is possible that the total solubility (both
physical and chemical) of CO2 and H2S become equal as is seen in Figure 12 at
313 K. From Figure 13 it can also be seen that with increasing temperatures the
difference in dissociation constants of CO2 and H2S becomes less. However, the
difference in physical solubility between CO2 and H2S increases with temperature.
As a result the total solubility of H2S in aqueous MDEA will be higher than in CO2 at
elevated temperature. This is in line with the equilibrium – loading simulations of the
E-EOS as can be seen in Figure 12.
4.4.2 Quaternary system H2S-MDEA-H2O-CH4
To study the influence of methane on the solubility of H2S in aqueous MDEA
additional parameters are required:
• Pure component parameters of methane ([6]);
• Molecular binary interaction parameters CH4-MDEA and CH4-H2O. Values for
these parameters were taken from Huttenhuis et al. [6];
• Molecular binary interaction parameter CH4-H2S. A value of 0.08 is taken as
stated in Section 4.3.4.4. The H2S solubility is not very sensitive to the value of
this parameter;
• Ionic binary interaction parameter CH4-MDEAH+. The value for this parameter
was taken from Huttenhuis et al. [6] and slightly modified in this chapter (refer to
Section 4.3.5.2).
120 Chapter 4
The electrolyte equation of state is compared with the experimental solubility data of
H2S in aqueous MDEA at different partial pressures methane as presented in
Appendix A of this thesis [5]. In this appendix experimental H2S solubility data are
presented in aqueous 35 – 50 wt.% MDEA at 283 and 298 K with methane as
make-up gas up to a methane partial pressure of 69 bar. In Appendix A it is
concluded from the experimental data, that the H2S solubility decreases with
increasing methane partial pressure. The experimental data in Appendix A, a total
of 30 experiments with varying temperatures, MDEA concentrations, H2S loadings
and CH4 partial pressures, are compared to the outcome of the E-EOS simulations.
The results are shown in Table 11.
data BIAS [%] AAD [%]
Overall 30 40 44
35 wt.% MDEA 12 17 26
50 wt.% MDEA 18 55 55
283 K 12 45 48
298 K 18 37 40
6.9 bar CH4 10 55 55
34.5 bar CH4 10 33 38
69 bar CH4 10 31 38
Table 11 Numbers of experimental data (Huttenhuis et al. [5]), BIAS and AAD for
the H2S solubility in aqueous MDEA and a methane partial pressure up to
69 bar
Table 11 shows that the model calculates significantly lower H2S partial equilibrium
pressures for all process conditions. The overall BIAS and AAD deviations for all 30
experimental data points are 40% and 44% respectively. Best results are found at
low temperature (283 K), low MDEA concentration (35 wt.%) and high methane
partial pressure (69 bar). When the results of these H2S-only experiments are
compared with the CO2–only work reported by Huttenhuis et al. [6], the same trends
H2S solubility in aqueous MDEA 121
are seen. Also in the CO2 work the model calculates lower acid gas partial
pressures. The model predictions at 35 wt.% MDEA are significantly better than the
predictions at 50 wt.% MDEA. This is also seen in the predictions for the system
H2S-MDEA-H2O reported in Section 4.4.1. However, model results of the CO2 work
with methane (overall BIAS 16%) are better than the H2S model calculations in this
chapter. It is concluded that the CO2-N2O analogy used by Huttenhuis et al. [6] to
regress the CO2-MDEA molecular binary interaction parameter may be less
applicable for higher MDEA concentrations. The same can be concluded for the
H2S-N2O analogy used in this chapter to regress the H2S-MDEA molecular binary
interaction parameter.
In Figure 14 the experimental H2S solubility as presented in Appendix A [5] is
compared with the calculations of the E-EOS model.
0.01
0.1
1
10
100
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4
Liquid loading [mole H2S / mole amine]
H2S
part
ial
pre
ssu
re [
kP
a]
6.9 bar; Huttenhuis et al. (2007) 6.9 bar (model)
34.5 bar; Huttenhuis et al. (2007) 34.5 bar (model)
69 bar; Huttenhuis et al. (2007) 69 bar (model)
Figure 14 Solubility of H2S in 50 wt.% MDEA at 298 K and different partial pressure
of methane
122 Chapter 4
This figure shows that the E-EOS predicts too low H2S solubilities over the entire
range. However, the influence of methane on the solubility is predicted correctly by
the model. If the partial pressure of methane increases the H2S solubility in aqueous
MDEA decreases.
In Figure 15 the partial pressure, fugacity and fugacity coefficient of H2S are
presented for a 35 wt.% MDEA solvent and a liquid loading of 0.1 as function of
methane partial pressure. From this figure it can be seen that the H2S partial
pressure is a strong function of the methane partial pressure. However, from Figure
15 it can also be seen that the H2S fugacity is more or less independent of the
methane partial pressure. So the reason for the decreasing H2S solubility at
increasing methane partial pressure is mainly the decreasing fugacity coefficient of
H2S. So it is expected that the model predictions will be improved by incorporating
additional experimental data from different research groups for the determination of
the interaction parameters. Especially experimental solubility data with methane are
lacking in literature The ionic interaction parameter MDEAH+-CH4 has been based
on experimental data of Addicks [7] and the molecular interaction parameter MDEA-
CH4 was based on data of Jou et al. [33].
H2S solubility in aqueous MDEA 123
0
0.2
0.4
0.6
0.8
1
1.2
0 20 40 60 80 100
Partial pressure methane [bar]
H2S
pa
rtia
l p
res
su
re / f
ug
ac
ity
[k
Pa
]
0
0.2
0.4
0.6
0.8
1
1.2
H2S
fu
ga
cit
y c
oe
ffic
ien
t [-
]
H2S partial pressure
H2S fugacity
H2S fugacity coefficient
Figure 15 Partial pressure, fugacity and fugacity coefficient of H2S in 35 wt.% MDEA
at 298 K at a liquid loading of 0.1 mole H2S / mole amine
4.5 Conclusions
In the present study an electrolyte equation of state model as developed in Chapter
3 [6] for the system CO2-MDEA-H2O-CH4 is further developed for the system H2S-
MDEA-H2O-CH4. The model has been validated with experimental solubility data of
H2S in aqueous MDEA in absence and presence of methane as a make-up gas. For
both the system H2S-MDEA-H2O and H2S-MDEA-H2O-CH4 the model under-
predicts the acid gas partial pressure (and over-predicts the acid gas solubility).
However, model predictions for the system in absence of methane are better. Both
experimental data and model calculations show that an increase in partial pressure
of methane results in a decrease of H2S solubility. It is concluded that this
124 Chapter 4
decreasing solubility is caused by a decreasing H2S fugacity coefficient at
increasing methane partial pressure. More experimental data are required to
improve the accuracy of the E-EOS. Especially additional acid gas solubility data
with high methane partial pressures are required, because in this study only one
single source could be used for model validations.
List of symbols
A Helmholtz energy [J]
AAD Absolute Average Deviation [%]
BIAS Mean BIAS Deviation [%]
d Coefficients for dielectric constant
g Interaction parameter in Huron-Vidal
mixing rule
[J.m-3
]
H Henry coefficient [kPa.m3.kmole
-1]
K Chemical equilibrium constant [-]
k Binary (molecular) interaction
parameter
[-]
MDEA N-methyldiethanolamine [-]
M Molar mass [gram.mol-1
]
n Mole number [mole]
P (partial) Pressure [Pa]
p1 ,p2, p3 Polarity parameters [-]
R Gas constant [J.mole-1
.K-1
]
T Temperature [K]
W Binary ionic interaction parameter [m3.mol
-1]
x Liquid mole fraction [-]
y Vapor mole fraction [-]
H2S solubility in aqueous MDEA 125
Greek symbols
� Binary nonrandomness parameter in
Huron-Vidal mixing rule
[-]
� Ionic/molecular diameter [m]
� Accentric factor [-]
Sub/super-scripts
∞ Infinite dilution
a Anion
aq. Aqueous
c Cation
C Critical
calc Calculated by model
exp Experiments
i,j Index
L Liquid
m Molecular
mix Mixture
R Reduced / residual
S Solvent
V Vapor
126 Chapter 4
References
[1] J. Schwarzentruber, H. Renon S. Watanasiri, Development of a new
Equation Of State for phase equilibrium calculations, Fluid Phase Eq., 52
(1989) 127-134.
[2] M.J. Huron, J. Vidal, New mixing rules in simple equations of state for
representing vapour-liquid equilibria of strongly non-ideal mixtures, Fluid
Phase Eq., 3 (1979) 255-271.
[3] W. Fürst, H. Renon, Representation of excess properties of electrolyte
solutions using a new equation of state, AIChE Journal, 39 (1993) 335-343.
[4] G. Vallée, P. Mougin, S. Jullian, W. Fürst, Representation of CO2 and H2S
absorption by aqueous solutions of diethanolamine using an Electrolyte
Equation of State, Ind. Eng. Chem. Res., 38 (1999) 3473-3480.
[5] P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Gas
solubility of H2S and CO2 in aqueous solutions of N-methyldiethanolamine,
Journal of Petroleum Science and Engineering, 55 (2007) 122-134
(Appendix A of this thesis).
[6] P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F. Versteeg, The solubility of
carbon dioxide in aqueous N-methyldiethanolamine solutions, Fluid Phase
Eq., 264 (2008) 99-112 (Chapter 3 of this thesis).
[7] J. Addicks, Solubility of carbon dioxide and methane in aqueous N-
methyldiethanolamine solutions at pressures between 100 and 200 bar,
Ph.D thesis, Norwegian University of Science and Technology (2002).
[8] D.M. Austgen, G.T. Rochelle, Model of vapor-liquid equilibria for aqueous
acid gas-alkanolamine systems. 2. Representation of H2S and CO2
solubility in aqueous MDEA and CO2 solubility in aqueous mixtures of
MDEA with MEA or DEA, Ind. Eng. Chem. Res., 30 (1991) 543-555.
[9] F.T. Selleck, L.T. Carmichael, B.H. Sage, Phase behavior in the hydrogen
sulfide-water system, Ind. Eng. Chem., 44 (1952) 2219-2226.
[10] J.I. Lee, A.E. Mather, Solubility of hydrogen sulfide in water, Berichte der
Bunsen-Gesellschaft, 81 (1977) 1020-1023.
H2S solubility in aqueous MDEA 127
[11] E.C.W. Clarke, D.N. Glew, Aqueous nonelectrolyte solutions. part VIII.
Deuterium and hydrogen sulfides solubilities in deuterium oxide and water,
Can. J. Chem., 49 (1971) 691-698.
[12] A. Jamal, Absorption and desorption of carbon dioxide and carbon
monoxide in alkanolamine systems, Ph.D thesis, University of British
Columbia (2002).
[13] G.F. Versteeg, W.P.M. van Swaaij, Solubility and diffusivity of acid gases
(CO2, N2O) in aqueous alkanolamine solutions, J. Chem. Eng. Data, 32
(1988) 29-34.
[14] N. Haimour, O.C. Sandall, Absorption of carbon dioxide into aqueous
Methyldiethanolamine, Chem. Eng. Sci., 39 (1984) 1791-1796.
[15] F.-Y. Jou, J.J. Carroll, A.E. Mather, F.D. Otto, Solubility of N2O in
methyldiethanolamine solutions, 9th IUPAC conference on Chemical
Thermodynamics (1986) Lisbon.
[16] Y.G. Li, A.E. Mather, Correlation and prediction of the solubility of N2O in
mixed solvents Fluid Phase Eq., 96 (1994) 119-142.
[17] H.K. Pawlak, R. Zarzycki, Solubility of carbon dioxide and nitrous oxide in
water + methyldiethanolamine and ethanol + methyldiethanolamine
solutions, J. Chem. Eng. Data, 47 (2002) 1506-1509.
[18] E.B. Rinker, O.C. Sandall, Physical solubility of hydrogen sulfide in several
aqueous solvents, Can. J. Chem. Eng., 78 (2000) 232-236
[19] R.C. Reid, J.M. Prausnitz, B.E. Poling, The Properties of Gases and
Liquids, fourth ed., McGraw-Hill, 1988.
[20] R.N. Maddox, A.H. Bhairi, J.R. Diers,., P.A. Thomas, GPA Research Report
RR-104 (1987).
[21] B. Lemoine, Y.-G. Li, R. Cadours, C. Bouallou, D. Richon, Partial vapor
pressure of CO2 and H2S over aqueous methyldiethanolamine solutions,
Fluid Phase Eq., 172 (2000) 261-277.
[22] S.H. Huang H.-J. Ng, GPA Research Report RR-155 (1998).
128 Chapter 4
[23] A. Perez-Salado Kamps, A. Balaban, M. Jödecke G. Kuranov N.A.
Smirnova, G. Maurer, Solubility of single gases carbon dioxide and
hydrogen sulfide in aqueous solutions of N-methyldiethanolamine at
temperatures from 313 to 393 K and pressures up to 7.6 MPa: new
experimental data and model extension, Ind. Eng. Chem. Res., 40 (2001)
696-706.
[24] G. Kuranov, B. Rumpf, N.A. Smirnova, G. Maurer, Solubility of single gases
carbon dioxide and hydrogen sulfide in aqueous solutions of N-
methyldiethanolamine in the temperature range 313-413 K at pressures up
to 5 MPa, Ind. Eng. Chem. Res., 35 (1996) 1959-1966.
[25] R.J. MacGregor, A.E. Mather, Equilibrium solubility of H2S and CO2 and
their mixtures in a mixed solvent, Can. J. Chem. Eng., 69 (1991) 1357-
1366.
[26] W.J. Rogers, J.A. Bullin, R.R. Davidson, FTIR Measurements of Acid-Gas-
Methyldiethanolamine Systems, AIChE J., 44 (1998) 2423-2430.
[27] R. Sidi-Boumedine, S. Horstmann, K. Fischer, E. Provost, W. Fürst, J.
Gmehling, Experimental determination of hydrogen sulfide solubility data in
aqueous alkanolamine solutions, Fluid Phase Eq., 218 (2004) 149-155.
[28] F.-Y. Jou, A.E. Mather, F.D. Otto, Solubility of H2S and CO2 in aqueous
methyldiethanolamine solutions, Ind. Eng. Chem. Process. Des., 21 (1982)
539-544.
[29] F.-Y. Jou, A.E. Mather, F.D. Otto, Solubility of carbon dioxide and hydrogen
sulfide in a 35 wt% aqueous solution of methyldiethanolamine, Can. J.
Chem. Eng., 71 (1993) pp. 264-268.
[30] M.-H. Li, K.-P. Shen, Solubility of hydrogen sulfide in aqueous mixtures of
monoethanolamine with n-methyldiethanolamine, J. Chem. Eng. Data, 38
(1993) 105-108.
[31] L. Chunxi, W. Fürst, Representation of CO2 and H2S solubility in aqueous
MDEA solutions using an electrolyte equation of state, Chem. Eng. Sc., 55
(2000) 2975-2988.
H2S solubility in aqueous MDEA 129
[32] M. L. Posey, G.T. Rochelle, A thermodynamic model of methyldiethanol-
amine-CO2-H2S-water, Ind. Eng. Chem. Res., 36, (1997) 3944-3953.
[33] F.-Y.Jou, J.J. Caroll, A.E. Mather, F.D. Otto, Solubility of methane and
ethane in aqueous solutions of methyldiethanolamine, J. Chem. Eng. Data.,
43 (1998) 781-784.
130 Chapter 4
131
Chapter 5
Solubility of Carbon Dioxide and
Hydrogen Sulphide in Aqueous
N-methyldiethanolamine
Abstract
In this chapter 72 experimental solubility data points of H2S and CO2 mixtures in
aqueous MDEA solutions at different methane partial pressures (up to 69 bar) are
presented. They are correlated using an electrolyte equation of state (E-EOS). This
model has already been used to estimate the CO2 solubility in aqueous MDEA
(P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F. Versteeg, Fluid Phase Eq. 264
(2008) 99-112) and the H2S solubility in aqueous MDEA (P.J.G. Huttenhuis, N.J.
Agrawal, G.F. Versteeg, Int. J. Oil, Gas and Coal Technology 1 (2008) 399-424).
Here the model is further extended to predict the behaviour of CO2 and H2S when
they are present simultaneously in aqueous MDEA. The application of an equation
of state is a new development for these acid gas – amine systems. The molecular
interactions are described by Schwarzentruber’s modification of the Redlich-Kwong-
132 Chapter 5
Soave equation of state, with terms are added to account for ionic interactions in the
liquid. The model is used to describe acid gas solubility data of the system CO2-
H2S-MDEA-H2O in open literature and the experimental data described here for the
system CO2-H2S-MDEA-H2O-CH4.
5.1 Introduction
Acid gases, such as CO2 and H2S are commonly present in natural gas. In the past,
research has focused on the development of solvents to remove H2S selectively
down to low gas concentrations (of less than 10 ppm). To lower the operational
costs for these processes, it was attractive not to remove the CO2. The H2S
concentration is usually much lower than the CO2 concentration, so selective
solvents were designed which show a high reaction rate with H2S and a low
reaction rate with CO2 (i.e. MDEA). However, because of the greenhouse effect,
research has recently been focused on the removal of CO2 from gas streams. The
acid components can be removed from the gas in many ways. However, the
removal with aqueous alkanolamine solutions in an absorber-desorber is most
commonly used. To predict mass transfer from gas to liquid and thus the
dimensions of the process equipment, the thermodynamics of the system need to
be known accurately.
In literature several thermodynamic models have been reported for alkanolamine –
acid gas systems. In this work an electrolyte equation of state (E-EOS) is used to
describe the system CO2-H2S-MDEA-H2O-CH4. This model has already been
applied to the systems CO2-MDEA-H2O-CH4 [1] and H2S-MDEA-H2O-CH4 [2].
To validate the E-EOS new experimental solubility data are required, which are
presented in Section 5.3.2. In total 72 new solubility experiments are presented for
the system CO2-H2S-MDEA-H2O-CH4. The influence of inert gas, in this case
methane, on the acid gas is studied quantitatively for typical natural gas conditions.
CO2 and H2S solubility in aqueous MDEA 133
Acid gas solubility data are usually limited to low pressures with no inert present;
sometimes low pressure (1 bar) nitrogen is used as a make-up gas. Here the acid
gas solubility (of CO2 and H2S simultaneously) is measured for system pressures up
to 69 bar with methane as the inert, make-up gas.
First, the E-EOS is briefly described. Then, the experimental method and solubility
results are presented. Then, the E-EOS is compared with data of the system CO2-
H2S-H2O-MDEA-H2O from open literature and to the new experimental data in the
presence of methane.
5.2 The electrolyte equation of state
In this study an electrolyte equation of state (E-EOS) is used to describe the system
CO2-H2S-MDEA-H2O-CH4. This system has already been developed for the single
acid gas systems in previous work [1], [2]. Schwarzentruber’s modification [3] of the
Redlich-Kwong-Soave EOS is used with a Huron-Vidal mixing rule [4]. To allow for
ions in the liquid additional (electrolyte) interactions are added to the molecular
equation of state. The E-EOS is based on a Helmholz energy which is a summation
of molecular and ionic interactions. This approach was originally proposed by Fürst
and Renon [5].
Posey [6] has found that mixed gas equilibria can be fairly well predicted with a
thermodynamic model using accurate single gas parameters. When CO2 and H2S
are present simultaneously, only one additional parameter is required compared
with the single gas E-EOS. Only the value of the CO2-H2S molecular interaction
parameter needs to be determined. This parameter was determined at a value of
0.12 (using the van der Waals mixing rule) by regressing the model with the
experimental data as described in Section 5.4.1. During simulations it appeared that
the results were not sensitive to the value of this parameter. The values for all the
134 Chapter 5
other parameters used in the E-EOS were identical to those for the single gas
systems. Reference is made to [7], [1] and [2].
5.3 Experimental
5.3.1 Experimental setup and procedure
The chemicals used in this study are described in the table below:
Name CAS-number Purity Supplier
N-methyldiethanolamine
(MDEA)
105-59-97 99+% Acros
Water (H2O) 7732-18-5 Demineralised
Hydrogen sulfide (H2S) 7783-06-4 99.6% Hoekloos
Carbon dioxide (CO2) 124-38-9 99.7 % Hoekloos
Methane (CH4) 74-82-8 99.5 % Hoekloos
Nitrogen (N2) 7727-37-9 99.99% Hoekloos
Table 1 Chemicals used in this study
For the experimental determination of the solubility a 1 dm3, intensively stirred Büchi
reactor is used. In this reactor it is possible to analyse the gas concentration and to
take liquid samples. The main parts of the reactor are:
• A gas supply: from this system a certain amount of CO2 and/or H2S can be
introduced;
• A reactor containing a stirrer, heating system and a liquid sampler;
• A gas analysis system: The H2S concentration in the gas phase is
measured in a Varian Micro GC CP-2003. The CO2 concentration is
measured with a MAIHAK S700 infrared analyser.
CO2 and H2S solubility in aqueous MDEA 135
A detailed description of the experimental procedures is given by Huttenhuis et al.
[7].
The H2S concentration in the liquid phase is measured with an automated
iodometric back titration using thiosulfate, while the CO2 concentration is measured
with a backtitration using TBAH. With the TBAH titration method the total amount of
acid gas (CO2 and H2S) is determined and not the amount of CO2 separately.
Therefore an excess amount of CuSO4 is added in a vessel containing boiling
sulphuric acid. In this way all sulfur species precipitate irreversibly as CuS, while the
amount of CO2 present is not influenced. In the single gas CO2 experiments, the
TBAH liquid titration method (without using CuSO4) appeared to be very accurate,
with results always within 10 % of the liquid loading determined from the amount of
CO2 added to the reactor. However, for the mixed gas experiments reported in this
work, the difference between the titration and the mass balance was more than 20%
for CO2. Therefore, it was decided to determine the CO2 liquid loading from the
mass balance instead of from titration with TBAH. With this method the accuracy in
the low loading range (<0.1 mole CO2 / mole amine) was estimated to be within
10% and in the high loading range (> 0.1 mole CO2 / mole amine) within 5 %.
5.3.2 Experimental results
Some initial experiments were carried out to validate the experimental procedures.
From these experiments it was concluded that the methods used were able to
produce both reliable H2S and CO2 solubility data in aqueous amine solvents. The
results of the experiments were well in line with literature sources.
In this work new experimental solubility data were obtained for two different solvents
(35 and 50 wt.% aqueous MDEA), at two temperatures (283 and 298 K) and at
three different system pressures (6.9, 34.5 and 69 bar) with methane as an inert
gas. In total 72 data points were produced on the following matrix:
136 Chapter 5
Temperature [K] 283 and 298
MDEA concentration [wt.%] 35 and 50
System pressure [bar] 6.9, 34.5 and 69
CO2 liquid loading [mol CO2 / mol amine] 0.05, 0.15 and 0.30
H2S gas concentration [ppm] 200 and 2000 1)
1) These gas concentrations are approximate; it was not possible to adjust them accurately
Table 2 Experimental matrix for the solubility experiments
The results of the solubility experiments are shown in Table 3, Table 4, Table 5 and
Table 6.
CO2 and H2S solubility in aqueous MDEA 137
P CO2 liquid loading P CO2 H2S liquid loading P H2S
[bar] [mol CO2/mol amine] [kPa] [mol H2S/mol amine] [kPa]
6.9 0.060 0.086 0.037 0.1511)
6.9 0.125 0.216 0.037 0.1971)
6.9 0.201 0.532 0.036 0.2781)
34.7 0.050 0.135 0.103 0.497
35.7 0.152 0.568 0.084 0.8031)
34.5 0.396 3.02 0.033 0.6101)
69.0 0.050 0.207 0.169 1.78
69.8 0.152 0.776 0.144 1.891)
70.1 0.300 2.08 0.082 1.95
6.9 0.061 0.180 0.145 1.001)
7.2 0.164 0.667 0.139 1.441)
7.0 0.325 2.07 0.143 2.241)
34.8 0.050 0.310 0.351 5.41
35.8 0.152 1.33 0.363 7.371)
35.0 0.325 3.42 0.245 6.861)
69.2 0.050 0.692 0.554 17.2
69.7 0.152 4.26 0.592 35.21)
70.0 0.325 7.57 0.468 22.71)
1)
These mixed gas experiments have been carried out with nitrogen as inert gas instead of methane.
The measured H2S gas concentration of these experiments in nitrogen have been corrected (multiplied
with factor 1.3) to simulate the results with methane as inert gas. For details reference is made to
Section 5.3.3.
Table 3 Experimental solubility data of CO2 and H2S simultaneously in 35 wt.%
MDEA at 283 K
138 Chapter 5
P CO2 liquid loading P CO2 H2S liquid loading P H2S
[bar] [mol CO2/mol amine] [kPa] [mol H2S/mol amine] [kPa]
6.9 0.050 0.278 0.025 0.188
6.9 0.150 1.49 0.019 0.243
7.0 0.300 3.93 0.016 0.280
34.7 0.050 0.308 0.051 0.572
34.6 0.150 3.90 0.275 8.90
34.6 0.300 5.22 0.023 0.546
70.1 0.050 0.421 0.085 1.42
68.3 0.150 1.78 0.085 2.00
69.0 0.300 5.81 0.088 3.69
7.0 0.050 0.42 0.089 1.04
7.0 0.150 1.87 0.091 1.49
6.9 0.300 1.30 0.061 1.46
34.5 0.050 0.759 0.251 6.80
34.7 0.150 3.19 0.195 5.67
34.5 0.300 5.97 0.127 5.02
69.6 0.050 1.51 0.380 15.2
69.8 0.150 3.32 0.253 9.99
69.9 0.300 10.12 0.246 14.9
Table 4 Experimental solubility data of CO2 and H2S simultaneously in 35 wt.%
MDEA at 298 K
CO2 and H2S solubility in aqueous MDEA 139
P CO2 liquid loading P CO2 H2S liquid loading P H2S
[bar] [mol CO2/mol amine] [kPa] [mol H2S/mol amine] [kPa]
7.0 0.050 0.131 0.024 0.127
6.9 0.150 0.760 0.020 0.200
7.1 0.300 2.11 0.012 0.126
35.0 0.050 0.182 0.046 0.392
34.6 0.150 0.872 0.032 0.398
35.7 0.300 2.88 0.029 0.532
68.6 0.050 0.322 0.128 1.72
68.3 0.150 1.11 0.063 1.11
69.2 0.300 3.29 0.050 1.23
6.9 0.050 0.228 0.122 1.17
7.0 0.150 0.810 0.066 0.760
7.0 0.300 2.68 0.049 0.807
34.5 0.050 0.531 0.364 8.56
36.8 0.150 1.60 0.223 4.88
35.1 0.300 3.91 0.158 4.44
69.0 0.050 0.863 0.446 18.49
69.0 0.150 3.02 0.404 16.44
69.0 0.300 6.97 0.302 15.40
Table 5 Experimental solubility data of CO2 and H2S simultaneously in 50 wt.%
MDEA at 283 K
140 Chapter 5
P CO2 liquid loading P CO2 H2S liquid loading P H2S
[bar] [mol CO2/mol amine] [kPa] [mol H2S/mol amine] [kPa]
7.0 0.050 0.621 0.021 0.194
6.9 0.150 3.04 0.014 0.25
7.0 0.300 12.7 0.007 0.201
34.5 0.050 0.64 0.035 0.58
34.5 0.150 3.46 0.023 0.549
34.9 0.300 8.84 0.019 0.795
68.8 0.050 0.805 0.054 1.16
69.0 0.150 3.71 0.035 1.10
69.2 0.300 10.53 0.029 1.38
7.0 0.050 0.813 0.056 0.940
7.0 0.150 3.22 0.038 0.845
7.1 0.300 14.7 0.028 0.951
34.8 0.050 1.33 0.167 5.14
34.6 0.150 4.46 0.094 3.53
34.9 0.300 10.0 0.069 3.10
69.9 0.050 1.49 0.218 9.47
68.7 0.150 5.27 0.153 7.41
69.4 0.300 14.9 0.154 11.3
Table 6 Experimental solubility data of CO2 and H2S simultaneously in 50 wt.%
MDEA at 298 K
5.3.3 Discussion
As mentioned in Table 3, the initial experiments were carried out with nitrogen as
make-up gas instead of methane. To check the influence of the type of inert gas,
nitrogen was sent through the reactor, followed by methane and then again by
nitrogen. It appeared that the switchover did not influence the CO2 gas partial
pressure. However, the H2S partial pressure was influenced at both high and low
H2S concentrations by the make up gas used. When using methane, the H2S partial
pressure was approximately 30 % higher than when using nitrogen. The
experiments using nitrogen as make-up gas instead of methane, have been marked
with a 1)
in Table 3. The measured H2S partial pressures in nitrogen have been
multiplied with a factor 1.3 to allow them to be compared with those using methane.
CO2 and H2S solubility in aqueous MDEA 141
It is very difficult to present the data graphically, as presented in the Tables 3 to 6.
Moreover, a comparison with literature data is not possible because, the presently
determined data are unique in its kind. Figure 1 shows the influence of the CO2
liquid loading on the H2S solubility. The H2S solubility data without CO2 are taken
from Huttenhuis et al. [2].
1
10
100
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 0.45 0.5
Liquid loading [mole H2S / mole amine]
H2S
pa
rtia
l p
res
su
re [
kP
a]
0.00 mole CO2 / mole amine
0.05 mole CO2 / mole amine
0.15 mole CO2 / mole amine
0.30 mole CO2 / mole amine
Figure 1 H2S solubility in 35 wt.% aqueous MDEA pre-loaded with 0, 0.05, 0.15 and
0.3 mole CO2 / mole amine at 298 K and 69 bar with methane as the make-
up gas
Figure 2 shows the CO2 solubility in aqueous MDEA as a function of the H2S liquid
loading.
For these experiments the acid gas partial pressure increases with temperature,
MDEA concentration, acid gas liquid loading and methane partial pressure. The
142 Chapter 5
effects are similar to those found for CO2-only and H2S-only. Additionally, it appears
that the H2S liquid loading decreases with increasing CO2 liquid loading at constant
H2S partial pressure. For example the H2S liquid loading capacity decreases from
0.449 to 0.246 mole H2S / mole amine, if the CO2 liquid loading is increased from 0
to 0.3 mole CO2 / mole amine (PH2S is 14.9 kPa, 35 wt.% MDEA, 298 K, 69 bar).
The same can be concluded for the CO2 solubility in aqueous MDEA. As can be
seen in Figure 2, the CO2 partial pressure increases with increasing H2S liquid
loading.
0.1
1
10
100
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35
Liquid loading [mole CO2 / mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
low H2S liquid loading
high H2S liquid loading
Figure 2 CO2 solubility in 35 wt.% aqueous MDEA pre-loaded with a low (<0.09
mole H2S / mole amine) and high (>0.24 mole H2S / mole amine)
concentration H2S at 298 K at 69 bar system pressure with methane as
make-up gas
CO2 and H2S solubility in aqueous MDEA 143
5.4 Model results
5.4.1 System CO2-H2S-MDEA-H2O
The E-EOS for the system CO2-H2S-MDEA-H2O has been validated with the
experimental solubility data in aqueous MDEA, when CO2 and H2S were present
simultaneously. The amount of experimental data for this system in open literature
is very limited. The following experimental solubility data were used to validate the
model:
• Huang and Ng [8]: Solubility of CO2 and H2S simultaneously in 50 wt.%
MDEA at 313 K and 373 K;
• Jou et al. [9]: Solubility of CO2 and H2S simultaneously in 35 wt.% MDEA at
313 K;
• Bullin et al. [10]: Solubility of CO2 and H2S simultaneously in 23 wt.% MDEA
at 313 and 323 K and 50 wt.% MDEA at 313 K.
The comparisons of the mixed gas VLE data from open literature, with the E-EOS
calculations are presented in Figure 3 (CO2 solubility) and Figure 4 (H2S solubility):
144 Chapter 5
1.0E-04
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
1.0E+04
1.0E-04 1.0E-03 1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02 1.0E+03 1.0E+04
Experimental PCO2 [kPa]
Calc
ula
ted
PC
O2 [
kP
a]
Jou et al. (1993)
Huang and Ng (1998)
Bullin et al. (1997)
Figure 3 Parity plot of the CO2 solubility for the system H2S-CO2-MDEA-H2O (refer
to [8], [9] and [10])
CO2 and H2S solubility in aqueous MDEA 145
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
1.0E-03 1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02 1.0E+03
Experimental PH2S [kPa]
Ca
lcu
late
d P
H2S [
kP
a]
Jou et al. (1993)
Huang and Ng (1998)
Bullin et al. (1997)
Figure 4 Parity plot of the H2S solubility for the system H2S-CO2-MDEA-H2O (refer
to [8], [9] and [10])
From Figure 3 and Figure 4 it appears that the model gives good predictions of the
solubility of mixed gases in aqueous MDEA. At low partial pressures (< 0.1 kPa) the
model seems to overpredict the acid gas partial pressure for both H2S and CO2.
Especially for CO2 the difference in the calculated and measured results of Bullin et
al. [10] is significant. This was also concluded by Posey [6], who used an NRTL
model to describe the same thermodynamic reactive system. In Table 7 the BIAS
and AAD deviations are given for the different sets of data. The BIAS and AAD
deviations are defined as follows:
,exp , ,exp ,
1 1,exp ,exp
1 1100% 100%
n n
i i calc i i calc
i ii i
y y y yAAD BIAS
n y n y= =
− −= ⋅ = ⋅� �
146 Chapter 5
BIAS H2S BIAS CO2 AAD H2S AAD CO2
number of points [%] [%] [%] [%]
Jou et al. (1993) 91 -34.5 -4.0 36.9 22.6
Huang and Ng. (1998) 16 -3.6 13.5 19.9 24.3
Bullin et al. (1997) 21 -26.1 -121.4 41.3 141.6
Bullin et al. (1997) corrected 1)
16 -40.5 -19.3 40.5 19.3
total 128 -26.6 -18.8 35.2 42.2
total corrected for Bullin data 1)
123 -27.3 0.6 36.3 23.6
1) 5 experimental data points of Bulin et al. with AAD > 250 % (CO2 solubil ity) were omitted
Table 7 AAD and BIAS deviation for the solubility of CO2 and H2S simultaneously in
aqueous MDEA
From Table 7 it can be seen that the predictions of the E-EOS differ considerably
from the CO2 solubility data of Bullin et al [10], i.e. the BIAS deviation for these data
is -121.4 %. Therefore the five experimental data points of Bulllin et al. were omitted
and new BIAS and AAD deviations were calculated. The accuracy of the CO2
solubility of the Bullin data increased significantly; i.e. the BIAS and AAD deviations
changed from -121.4 % to -19.3 % and from 141.6 % to 19.3 % respectively. The
deletion of these five data points also resulted in increased deviations of the total
experimental data set containing data of Huang and Ng [8], Jou et al. [9] and Bullin
et al [10].
The total BIAS deviation (corrected for Bullin data) of the H2S solubility data is
-27.3%, so the model overpredicts the H2S partial pressure. This is not in line with
the H2S-only experiments (without CO2) were a BIAS deviation of + 2% was found
by Huttenhuis et al. [2]. However, the BIAS deviation of the data of Huang and Ng.
[8] is only -3.6 %. The quality of the CO2 experimental data is much better. The
BIAS deviation (corrected for Bullin data) is 0.6 %. However, there is some variation
between the different research groups, because the BIAS is -19.3 % for the
(corrected) Bullin data, while for the Huang and Ng. data the BIAS deviation is
+13.5 %.
CO2 and H2S solubility in aqueous MDEA 147
5.4.2 System CO2-H2S-MDEA-H2O-CH4
The electrolyte equation of state is further used to describe the experimental
solubility data of the system CO2-H2S-MDEA-H2O-CH4 as presented in Section
5.3.2. In Figure 5 and Figure 6, these CO2 and H2S solubility data are compared
with the E-EOS.
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02
Experimental PCO2 [kPa]
Ca
lcu
late
d
PC
O2 [
kP
a]
35 wt.%; 283 K
35 wt.%; 298 K
50 wt.%; 283 K
50 wt.%; 298 K
Figure 5 Parity plot of the CO2 solubility for the system CO2-H2S-MDEA-H2O-CH4
(this work)
148 Chapter 5
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E-02 1.0E-01 1.0E+00 1.0E+01 1.0E+02
Experimental PH2S [kPa]
Ca
lcu
late
d
PH
2S [
kP
a]
35 wt.%; 283 K
35 wt.%; 298 K
50 wt.%; 283 K
50 wt.%; 298 K
Figure 6 Parity plot of the H2S solubility for the system CO2-H2S-MDEA-H2O-CH4
(this work)
The BIAS and AAD deviations of the system CO2-H2S-MDEA-H2O-CH4 are
presented in Table 8.
BIAS H2S BIAS CO2 AAD H2S AAD CO2
number of points [%] [%] [%] [%]
35 wt.% MDEA; 283 K 18 4.5 -8.7 25.9 24.3
35 wt.% MDEA; 298 K 18 26.3 5.8 26.3 30.7
50 wt.% MDEA; 283 K 18 37.7 33.0 41.8 41.3
50 wt.% MDEA; 298 K 17 48.9 53.1 48.9 53.1
total 71 29.1 20.4 35.5 37.1
Table 8 AAD and BIAS deviation for the solubility of CO2 and H2S in the system
CO2-H2S-MDEA-H2O-CH4
CO2 and H2S solubility in aqueous MDEA 149
From Figure 5, Figure 6 and Table 8 it can be concluded that both the solubility of
H2S and CO2 in aqueous MDEA is predicted better by the E-EOS in 35 wt.%
aqueous MDEA than in 50 wt.% MDEA. The same conclusion was made for the
experiments with CO2–only [1] and H2S–only [2]. In [1] and [2] it was suggested that
the H2S-N2O and CO2-N2O analogy used in the model to calculated the binary
interaction parameters of the system H2S-MDEA and CO2-MDEA, is not applicable
at high amine concentrations. Kierzkowska-Pawlak and Zarzycki [11] studied the
applicability of the CO2 and N2O analogy in a MDEA – ethanol system. In this
system both the N2O and CO2 dissolve physically only, because no chemical
reaction can take place between the CO2 and the solvent. In this study it was
concluded that the CO2-N2O analogy is not applicable over the whole amine
concentration. The N2O solubility into ethanol solutions of MDEA decreases with the
rise of amine concentration while the CO2 solubility increases. So again it appears
that attention should be paid to this CO2-N2O analogy at high amine concentrations.
It can also be seen that the predictions at 283 K are better than at 298 K. This was
also found for the H2S–only experiments in the system H2S-MDEA-H2O-CH4 [2].
In Chapter 3 and Chapter 4 the influence of methane on the H2S and CO2 solubility
in aqueous MDEA was studied quantitatively CO2-only [1] and H2S-only [2]. It was
concluded that the acid gas solubilities decreased with increasing methane partial
pressure. The reason was thought to be the decreasing acid gas fugacity coefficient
with increasing methane partial pressure. Simulations with the E-EOS have been
carried out to study the influence of CH4, CO2 and H2S on the acid gas solubility in
aqueous MDEA in case CO2 and H2S are present simultaneously. From the
experimental data presented in this work (refer to Section 5.3.2), the influence of
methane on the acid gas solubility could not be derived directly, because the
experiments have been carried out with a constant H2S gas phase concentration,
instead of a constant H2S partial pressure. In Table 9 the (acid) gas partial
pressures, fugacity and fugacity coefficients are summarized for the different
simulations:
150 Chapter 5
CO2 loading H2S loading PCH4 PH2S PCO2 fH2S fCO2 �H2S �CO2
[mol CO2/mol amine] [mol H2S/mol amine] [bar] [kPa] [kPa] [kPa] [kPa] [-] [-]
0.1 0.1 6.9 0.98 0.70 0.94 0.68 0.967 0.972
0.1 0.1 34.5 1.17 0.83 0.99 0.72 0.845 0.866
0.1 0.1 69 1.46 1.01 1.05 0.76 0.715 0.751
0.1 0.3 6.9 6.42 1.56 6.20 1.51 0.967 0.972
0.1 0.3 34.5 7.71 1.84 6.51 1.59 0.845 0.866
0.1 0.3 69 9.67 2.26 6.91 1.69 0.714 0.751
0.3 0.1 6.9 2.14 4.56 2.07 4.43 0.967 0.972
0.3 0.1 34.5 2.57 5.39 2.17 4.66 0.845 0.866
0.3 0.1 69 3.22 6.62 2.30 4.97 0.715 0.751
0.3 0.3 6.9 12.25 8.69 11.83 8.44 0.966 0.972
0.3 0.3 34.5 14.74 10.29 12.44 8.91 0.844 0.865
0.3 0.3 69 18.54 12.67 13.24 9.51 0.714 0.750
fugacity coefficientpartial pressure fugacity
Table 9 CO2 and H2S solubility in 35 wt.% aqueous MDEA at 298 K as calculated by
the E-EOS
In Figure 7 the partial pressures and fugacity coefficients of H2S and CO2 as
calculated with the E-EOS are presented as function of methane partial pressure for
constant acid gas loading.
CO2 and H2S solubility in aqueous MDEA 151
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
0 10 20 30 40 50 60 70 80
Partial pressure methane [bar]
ac
id g
as
pa
rtia
l p
res
su
re
0.0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1.0
ac
id g
as
fu
ga
cit
y c
oe
ffic
ien
t
CO2 partial pressure
H2S partial pressure
CO2 fugacity coefficient
H2S fugacity coefficient
Figure 7 H2S and CO2 acid gas fugacity coefficient as function of the methane
partial pressure as calculated by the E-EOS for the CO2-H2S-MDEA-H2O-
CH4 system; CO2 liquid loading is 0.1 mole/mole amine; H2S liquid loading
is 0.1 mole/mole amine; 35 wt.% aqueous MDEA; 298 K
The fugacity coefficients of both H2S and CO2 decrease with increasing methane
partial pressure, while the acid gas partial pressure increases. At low methane
partial pressures the fugacity coefficients approaches unity. The influence of the
methane partial pressure on the H2S fugacity coefficient is slightly higher than for
the CO2 coefficient. As was concluded by Huttenhuis et al. [1] and Huttenhuis et al.
[2], a lower acid gas fugacity coefficient results in a higher acid gas partial pressure
and thus a lower acid gas solubility. So, it may be concluded that also in the mixed
gas experiments the acid gas solubility decreases with increasing methane partial
pressure. The solubility of H2S is more affected by the increasing methane partial
152 Chapter 5
pressure, than the solubility of CO2, i.e. at a methane partial pressure of 69 bar the
H2S fugacity coefficient is 0.715, while the CO2 fugacity coefficient equals 0.751
(see Table 9).
Table 9 shows also the calculated results for higher CO2 and H2S loadings (0.3
instead of 0.1 mol acid gas / mol amine). It appears that there is no influence of the
acid gas liquid loading on the acid gas fugacity coefficient, when the acid gas liquid
loading is increased from 0.1 to 0.3 mol acid gas / mol amine. The H2S and CO2
fugacity coefficients at a H2S and / or CO2 liquid loading of 0.1 mol acid gas / mol
amine are the same for liquid loadings of 0.3 mol / mol. However, it should be noted
that the H2S solubility decreases with increasing CO2 liquid loading and vice versa
(see Figure 1 and Figure 2), because part of the amine capacity is consumed by the
acid gas.
5.5 Conclusions
In this study the solubilities of CO2 and H2S when present simultaneously in
aqueous MDEA have been studied experimentally and theoretically. This is with
methane acting as inert component. 72 new datapoints are presented for 35 and 50
wt.% aqueous MDEA at 283 and 298 K. The methane partial pressure has been
varied from 6.9 up to 69 bar. The H2S partial pressure increases significantly with
increasing CO2 liquid loading, i.e. the capacity of the solvent for H2S capture
decreases. During the experiments it appeared that the type of inert gas (nitrogen or
methane) did influence the H2S solubility. However, the CO2 partial pressure was
not influenced by the type of inert gas.
The experimental results were compared with an electrolyte equation of state which
describes both gas and liquid. The equation has terms to account for ionic species
which are present in the liquid. Calculations with this E-EOS show that the fugacity
coefficient of H2S is more sensitive to an increasing methane partial pressure than
CO2 and H2S solubility in aqueous MDEA 153
the fugacity coefficient of CO2. By Huttenhuis et al. [1] and Huttenhuis et al. [2] it
was concluded that a decreasing acid gas fugacity coefficient was responsible for
the decreasing acid gas solubility with increasing methane partial pressure. A
probable explanation for the effect inert gas type on CO2 and H2S is that the
fugacity coefficient of H2S is more sensitive to the inert gas type (nitrogen or
methane) than the fugacity coefficient of CO2. However, the influence of the type of
inert gas on the acid gas solubility needs to be studied further.
The E-EOS developed here was compared with experimental data in open literature
for the system CO2-H2S-MDEA-H2O. The scatter in the different sets of data is fairly
high. Therefore, more solubility experiments need to be carried out, where CO2 and
H2S are present simultaneously. The BIAS deviations for CO2 and H2S with the E-
EOS are respectively 0.6 % and - 27.3 %.
The E-EOS was also compared with experimental data of the system CO2-H2S-
MDEA-H2O-CH4 from this work (Section 5.3.2). The BIAS deviations for CO2 and
H2S are 20.4 and 29.1 %. Predictions at low MDEA concentration (35 wt.%) and low
temperature (283 K) are better than at higher MDEA concentration and
temperature. The influence of inert gas type on this acid gas solubility needs to be
studied in more detail.
List of symbols
AAD Absolute Average Deviation [%]
BIAS Mean BIAS Deviation [%]
MDEA N-methyldiethanolamine
E-EOS Electrolyte Equation Of State
TBAH Tert Butyl Alcohol
154 Chapter 5
References
[1] P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F. Versteeg, The solubility of
carbon dioxide in aqueous N-methyldiethanolamine solutions, Fluid Phase
Eq., 264 (2008) 99-112 (Chapter 3 of this thesis).
[2] P.J.G. Huttenhuis, N.J. Agrawal, G.F. Versteeg, The solubility of hydrogen
sulfide in aqueous N-methyldiethanolamine solutions, Int. J. Oil, Gas and
Coal Techn, 1 (2008) 399-424 (Chapter 4 of this thesis).
[3] J. Schwarzentruber, H. Renon S. Watanasiri, Development of a new cubic
equation of state for phase equilibrium calculations, Fluid Phase Eq., 52
(1989) 127-134.
[4] M.J. Huron, J. Vidal, New mixing rules in simple equations of state for
representing vapour-liquid equilibria of strongly non-ideal mixtures, Fluid
Phase Eq., 3 (1979) 255-271.
[5] W. Fürst, H. Renon, Respresentation of excess properties of electrolyte
solutions using a new equation of state, AIChE Journal, 39 (1993) 335-343.
[6] M.L. Posey, Thermodynamic model for acid gas loaded aqueous
alkanolamine solutions, PhD. thesis, University of Texas (1996).
[7] P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Gas
solubility of H2S and CO2 in aqeous solutions of N-methyldiethanolamine, J.
Pet. Sci. Eng., 55 (2007) 122-134 (Appendix A of this thesis).
[8] S.H. Huang, H.-J. Ng, GPA Research Report RR-155, (1998).
[9] F.-Y. Jou, J.J. Caroll, A.E. Mather, F.D. Otto, Solubility of mixtures of
hydrogen sulfide and carbon dioxide in aqueous N-Methyldiethanolamine
solutions, J. Chem. Eng. Data, 38 (1993) 75-77.
[10] J. Bullin, R. Davison, W. Rogers, GPA Research report RR-165, (1997).
[11] H. Kierzkowska-Pawlak, R. Zarzycki, Solubility of carbon dioxide and nitrous
oxide in water + methyldiethanolamine and ethanol + methyldiethanolamine
solutions, J. Chem. Eng. Data, 47, (2002) 1506-1509.
155
Appendix A
Solubility of H2S and CO2 in Aqueous
Solutions of N-methyldiethanolamine
Abstract
Alkanolamines are used in the industry to remove acid gases such as CO2 and H2S
from natural and industrial gas streams. The acid components react with the basic
alkanolamine via an exothermic, reversible reaction in a gas/liquid absorber. The
composition of these amine solutions is continuously changed to optimise the
(selective) removal of the several acid components. For the design of gas treating
equipment mass transfer, reaction kinetics and solubility data of acid gases in
aqueous alkanolamine solutions are required. In this appendix new solubility data of
H2S and CO2 in aqueous MDEA at different conditions encountered in modern gas
treating facilities are presented. The experimental pressures are varied from 6.9 to
69 bar (methane is used as make-up gas) and temperatures from 283 to 298 K. The
measured values are evaluated and correlated with an electrolyte equation of state
(E-EOS) as originally proposed by Fürst and Renon [Fürst, W., Renon, H., 1993.
Representation of Excess Properties of Electrolyte Solutions Using a New Equation
of State. AIChE J., 39 (2), pp. 335.]. The application of an equation of state for the
156 Appendix A
prediction of solubilities for reactive, ionic systems is a new development in this
field.
A.1 Introduction
Acid gases such as CO2, H2S and other sulphuric components are often present in
natural and industrial gases. They may have to be removed (selectively) from these
gas streams for operational, economical or environmental reasons. A commonly
used process is absorption in aqueous alkanolamine solvents. Here the acidic
components react with the alkanolamine in a gas/liquid contactor. The acidic
components are then removed from the solvent in a regenerator, usually at a low
pressure and/or high temperature. For the design of such processes reliable
solubility data are indispensable. In this appendix newly obtained solubility data of
CO2 and H2S in aqueous MDEA solutions will be presented.
The ability of an alkanolamine solution to remove acidic gases is determined by the
acid gas solubility, the reaction rate and the mass transfer properties. This study
considers the solubility of CO2 and H2S in aqueous MDEA at temperatures of 283
and 298 K, acid gas partial pressures 0.05-1000 kPa and a total system pressure of
6.9-69 bar with methane as make-up gas. In literature usually only the partial
pressure acid gas is specified and not the total system pressure, because
experiments are carried out at low pressure. In this thesis the influence of the total
system pressure (with methane as make-up gas) on the acid gas solubility is also
studied. This system pressure is an important parameter, because there usually is a
substantial difference in system pressure between an industrial absorber (70-100
bar) and a regenerator (2-3 bar). So if the system pressure influences the acid gas
solubility, the low pressure experimental solubility data cannot be used in the high
pressure absorber. Also measurements of the acid gas solubilities at low
temperatures of 283 and 298 K are scarce. The new solubility data are used to
Appendix A 157
develop an electrolyte equation of state (E-EOS) that can be used to predict the
equilibria for these treating processes.
A.2 Experimental
For all experiments demineralised water was used. N-methyldiethanolamine (purity
> 99%) was supplied by Acros; hydrogen sulfide (purity > 99.6%), carbon dioxide
(purity > 99.7%) and methane (purity > 99.5%) were supplied by Hoekloos.
For the determination of the gas solubility data a stirred, 1 litre, Büchi reactor was
used. The reactor system is shown in Figure 1. From this reactor both gas and
liquid samples are withdrawn and analysed.
continuous
methane
sweep flow
cooling water
reactor outlet to
gas chromatograph
/ offgas treatmentPITI
liquid sample
cooling water
H2S/CO
2 pre-loading
from gas bomb
to vacuum pump
sight glass
Figure 1 Reactor of the experimental set-up
158 Appendix A
The experimental set-up consists of three parts:
• A gas supply system: From this section the gases are supplied to the
reactor batchwise or continuously;
• A reactor section: this section contains a heating bath, a high intensity
stirrer (stirrer speed > 1000 rpm) and a liquid sampling system;
• Gas outlet system: this system contains a gas analyser, off-gas treatment
and a vacuum pump.
With this set-up it is possible to measure the total H2S and CO2 concentration in
both the gas and the liquid independently. As it is also possible to determine the
total amount of added H2S or CO2 added to the reactor, a mass balance check can
be made to determine the accuracy of the experiments.
During an experiment the reactor is filled with approximately 0.5 litre of aqueous
amine solution and evacuated until the vapor pressure of the solution is reached. A
predefined amount of acid gas is sent to the reactor. The partial pressure of
methane is increased to the required total system pressure. Under intensive stirring
of the reactor, a small sweep stream of methane (approximately 200 Nml min-1
) is
passed through the reactor and the outlet is analysed using a gas chromatograph.
When equilibrium is reached the reactor is blocked, a small liquid sample is taken,
and the amount of acid gas is analysed with a suitable liquid titration technique. The
CO2 content is measured with an automated organic acid-base titration and the H2S
content is measured with an automated iodometric back titration with thiosulfate.
The liquid sample containing CO2 is added to a vessel containing boiling sulfuric
acid. The high acidity and high temperature and addition of a small nitrogen purge
flow cause that the CO2 to be completely stripped from the sample. A reflux cooler
is used to prevent contamination of CO2 with sulfuric acid and water. The CO2 is
sent to a second vessel containing MEA and an organic solvent (DMF). In this
vessel the CO2 is captured by the MEA and subsequently the pH falls. The total
amount of CO2 is determined by keeping the MEA solution at its original pH with a
Appendix A 159
strong base (TBAH). For he determination of the amount H2S in the liquid sample,
an excess amount of iodine is added. The excess iodine is determined by a sodium
thiosulphate titration. Both titration methods are calibrated extensively with samples
containing a known amounts of Na2CO3 and Na2S.
When the acid gas partial pressure and liquid loading are determined a consecutive
experiment at a higher liquid loading is started. The reactor is depressurized and
an additional amount of acid gas from the gas supply vessel is added. For each
experiment it is verified that the amount of acid gas removed during the
depressurizing phase is negligible compared to the total amount of acid gas
absorbed by the alkanolamine solution.
A.3 Results
A.3.1 Experiments with CO2
To establish the accuracy of the experimental technique, set-up and procedures,
some validation experiments have been carried out and the results are compared
with CO2 solubility data available in the literature. The validation experiments have
been carried out with a 20 wt.% aqueous diethanolamine (DEA) solution at 323 K,
because at these conditions a large amount of experimental data are available. The
experimental results are compared to data of Haji-Sulaiman [7], [8], Bullin [4] and
Lee [16]. The comparison is presented in Figure 2.
160 Appendix A
0.001
0.01
0.1
1
10
100
0.01 0.1 1
Liquid loading [moleCO2/mole amine]
CO
2 p
art
ial
pre
ssu
re [
kP
a]
Haji-Sulaiman (1998)
Bullin (1997)
Haji-Sulaiman (1996)
Bullin (1997)
Lee (1974)
this work
Figure 2 Validation experiments for the solubility of CO2 in 20 wt.% DEA at 323 K
Figure 2 shows some scatter in literature data of the different authors. The newly
obtained values are in good agreement with the other data. At high liquid loadings
(> 0.4 mole/mole) the measured CO2 partial pressure is lower than measured by
Haji-Sulaiman [8] and Lee [16]. However, most of the experiments presented in the
present study were carried out at lower liquid loadings. The data of Lee [16] show
substantial deviations in the low loading range. From Figure 2, it can be concluded
that our experimental set-up is able to reproduce existing results of the CO2-DEA-
H2O system.
New solubility data of CO2 were obtained for two different amine solutions (35 and
50 wt.% MDEA) at two temperatures (283 and 298 K) and three system pressures
(6.9, 34.5 and 69 bar) with methane as make-up gas. The data are given in Table 1
(35 wt.% MDEA) and Table 2 (50 wt. % MDEA).
Appendix A 161
T = 283 K T = 298 K
P [bar] � [mole/mole] PCO2 [kPa] P [bar] � [mole/mole] PCO2 [kPa]
6.9 0.048 0.054 6.9 0.048 0.170
0.143 0.314 0.048 0.168
0.276 1.000 0.143 1.001
0.325 1.324 0.270 3.037
34.5 0.143 0.385 34.5 0.048 0.198
0.275 1.237 0.048 0.195
0.319 1.658 0.143 1.204
69.0 0.140 0.482 0.276 3.728
0.275 1.448 0.327 4.815
0.320 2.141 69.0 0.047 0.245
0.047 0.235
0.143 1.340
0.279 4.408
0.316 6.121
Table 1 Experimental solubility data of CO2 in an aqueous solution of 35 wt.%
MDEA
162 Appendix A
T = 283 K T = 298 K
P [bar] � [mole/mole] PCO2 [kPa] P [bar] � [mole/mole] PCO2 [kPa]
6.9 0.144 0.671 6.9 0.047 0.441
0.270 1.754 0.111 2.379
0.428 3.848 0.139 2.143
34.5 0.150 0.781 0.238 7.206
0.273 2.103 0.265 5.492
0.428 5.036 0.287 7.773
69.0 0.152 0.939 0.424 37.07
0.275 2.695 0.551 70.29
0.409 5.887 0.700 212.6
34.5 0.048 0.487
0.141 2.698
0.272 7.315
0.887 180.7
0.936 986.8
1.105 351.4
69.0 0.047 0.570
0.128 3.092
0.272 8.720
Table 2 Experimental solubility data of CO2 in an aqueous solution of 50 wt.%
MDEA
A.3.2 Experiments with H2S
The first validation runs were carried out with 50 wt.% MDEA at 313 K and 3.5 bar
(with nitrogen as make-up gas). The results of these experiments are compared
with literature data from Huang [9], Rogers [23] and Jou [11] in Figure 3.
Appendix A 163
0.01
0.10
1.00
10.00
0.01 0.10 1.00
Liquid loading [mole H2S/mole amine]
H2S
part
ial p
ressu
re [
kP
a]
Huang (1998)
Roger (1998)
Jou (1993)
this work
Figure 3 Validation experiments for the solubility of H2S in 50 wt.% MDEA at 313 K
The literature data from Jou [11] differ significantly from the other sources and our
new data. They also show a different trend in the low loading range. For this reason,
the accuracy of these data is questionable. A possible explanation of the differences
is the influence of contaminations (primary and/or secondary amines) on the
solubility of aqueous MDEA. However, if this is the reason, the effect should be
vanished at higher liquid loadings and this is not the case.
New solubility of H2S were obtained for two different blends (35 and 50 wt.%
MDEA) at two temperatures (283 and 298 K) and three pressure (6.9, 34.5 and 69
bar). The experimental data are given in Table 3 (35 wt.% MDEA) and Table 4 (50
wt. % MDEA).
164 Appendix A
T = 283 K T = 298 K
P [bar] � [mole/mole] PH2S [kPa] P [bar] � [mole/mole] PH2S [kPa]
6.9 0.052 0.141 6.9 0.042 0.156
0.171 1.057 0.165 1.495
34.5 0.112 0.638 34.5 0.102 0.707
0.575 14.976 0.391 8.542
69.0 0.172 1.691 69.0 0.144 1.745
0.574 18.982 0.449 14.838
Table 3 Experimental solubility data of H2S in an aqueous solution of 35 wt.% MDEA
T = 283 K T = 298 K
P [bar] � [mole/mole] PH2S [kPa] P [bar] � [mole/mole] PH2S [kPa]
6.9 0.081 0.486 6.9 0.028 0.153
0.125 1.137 0.062 0.609
34.5 0.095 0.828 0.083 1.024
0.365 8.349 0.105 1.484
69.0 0.132 1.760 34.5 0.028 0.179
0.447 17.250 0.062 0.727
0.083 1.19
0.230 6.51
69.0 0.028 0.21
0.062 0.856
0.083 1.411
0.366 12.715
Table 4 Experimental solubility data of H2S in an aqueous solution of 50 wt.%
MDEA
A.3.3 Discussion
From the CO2 and H2S data the following observations can be made. The acid gas
partial pressure increases (solubility decreases) with:
• increasing liquid loading (and constant temperature, pressure and amine
concentration);
• increasing temperature (and constant liquid loading, pressure and amine
concentration);
• increasing amine concentration (and constant temperature, pressure and
liquid loading.
Appendix A 165
1 2
R R R R R R
RF SR SR LR BORN
A A A A A A
RT RT RT RT RT RT
� � � � � � � � � � � �= + + + +� � � � � � � � � � � �
� � � � � � � � � � � �
These observations agree with data presented by other authors in this field.
It can also be concluded that the solubility of H2S and/or CO2 is substantially
affected by the methane partial pressure. Increasing the methane partial pressure
results in a pronounced decrease of the solubility of the acidic component. This is
line with the results of the experiments carried out by Addicks [1]. He measured the
solubility of CO2 and CH4 in aqueous MDEA at pressures up to 200 bar. At this time
it is not known whether the changing acid gas solubility is caused by the increased
system pressure or by the presence of methane in the system.
A.4 Validation of the model
A.4.1 Model description
The experimental results are compared with an electrolyte equation of state (E-
EOS), originally proposed by Fürst and Renon [6]. In this model the same equations
are used for both the liquid and vapor. The model can be extrapolated and the
speciation of the components in the liquid can be calculated. Moreover the solubility
of physically dissolved hydrocarbons (such as methane) can be calculated. This is
important for the design of high pressure gas treating equipment and for mass
transfer calculations.
The model used in the present study was originally developed by Solbraa [26].
Details of the model can be found in his work. His electrolyte equation of state is
derived from an expression of the Helmholtz energy (Equation 1) with non-
electrolyte parts (RF and SR1) and an electrolyte parts (SR2, LR and BORN).
Equation 1
166 Appendix A
The first two terms describe repulsive forces (RF) and attractive short range
interactions (SR1) in the molecular part of the equation of state. This model was
based on a cubic equation of state (Schwarzentruber’s [25] modification of the
Redlich-Kwong EOS with a Huron-Vidal mixing rule). The important parameters of
this part of the model are the critical properties, Schwarzentruber parameters and
molecular (Huron-Vidal) interaction parameters. These molecular interaction
parameters are determined by fitting experimental molecular binary data to the EOS
model.
To account for ions, three ionic terms are included; a short-range ionic term (SR2),
a long range ionic term (LR) and a Born term. The most important parameters in
SR2 are the molecular and ionic diameter and the ionic binary interaction
parameters. These ionic interaction parameters are determined by fitting the E-EOS
with experimental solubility data for the system CO2-MDEA-H2O. In this thesis only
the cation-molecules and cation-anion interactions are taken into account. The most
important parameter of the LR term is the dielectric constant of the solvent.
A Born term has been added to correct the standard states of ions. This term gives
the solvation energy of an ion in a dielectric medium, relative to vacuum. The Born
term is important for modelling both liquid and vapor with an E-EOS, because this
parameter causes the ions to stay mainly in the liquid. Fürst and Renon [6] did not
use the Born term in their original publication, but it was added in a later paper on
LLE in electrolyte systems (Zuo [30]). Solbraa [26] developed his E-EOS for a CO2-
MDEA-water system. The model was also validated by Solbraa for a high pressure
system (100-200 bar) of CO2-MDEA-water-methane. In this E-EOS the following
parameters have to be obtained:
• Molecular and ionic pure component parameters, such as critical data and
polar parameters. These data are independent of the model and can be
found in literature;
• Binary and ionic interactions parameters. These parameters are part of the
model and have to be determined via fitting procedures or from estimations.
Appendix A 167
2
2 2 3 3 3
2 2 2
2
2
' '
CO H O HCO H HCO CO H
H O OH H RR NH RR N H
H S HS H HS S H
− + − − +
− + + +
− + − − +
+ ←⎯→ + ←⎯→ +
←⎯→ + ←⎯→ +
←⎯→ + ←⎯→ +
The following chemical reactions occur in an aqueous MDEA solution when CO2
and H2S are present:
Here R corresponds to a methyl group and R’ to an ethanol group.
A.4.2 Validation of the Solbraa model
The results of the CO2 experiments in this appendix have been compared with the
E-EOS of Solbraa [26]. A large systematic deviation is observed between the
experimental results and the predictions of the E-EOS. The E-EOS always under-
estimates the CO2 partial pressure. The AAD and BIAS deviations of these
experiments are both 40%.
,exp , ,exp ,
1 1,exp ,exp
1 1100% 100%
n n
i i calc i i calc
i ii i
y y y yAAD BIAS
n y n y= =
− −= ⋅ = ⋅� �
In the following sections, the reason for this difference is discussed. In Figure 4 the
influence of the methane partial pressure can be seen for both the experiments and
the E-EOS.
168 Appendix A
0
0.5
1
1.5
2
2.5
3
0 20 40 60 80
System pressure [bar]
CO
2 p
art
ial p
res
su
re [
kP
a]
experiments
model results
Figure 4 Influence of the partial pressure of methane for the E-EOS and
experiments for CO2-MDEA-H2O-CH4 (T=283 K, 50 wt.% MDEA, liquid
loading=0.27 mole CO2 / mole amine)
From Figure 4 it can be concluded that the slopes of both graphs (influence of
methane partial pressure) are almost similar, a proportional relation exists between
total system pressure and the CO2 partial pressure. However, the intercept with the
y-axis is much higher for the experiments than calculated by the model. The results
at a system pressure of zero bar can be compared with results at zero partial
pressure of methane. It appears that the large deviations between model and
experiments are not caused by the input parameters and properties of methane in
the model, but by the parameters used for the ternary system CO2-MDEA-water.
For this reason the determination of the ionic parameters of the CO2-MDEA-water
system as carried out by Solbraa [26] was critically reviewed. The relevant ionic
parameters in this system were fitted against experimental data available in
literature.
Appendix A 169
A.4.3 Influence of experimental database
Figure 5 shows an overview of available CO2 solubility data in 50 wt.% MDEA at
313 K.
1.0E-05
1.0E-04
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
0.001 0.01 0.1 1
Liquid loading [mole CO2/mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
50 wt% Rogers (1998)
50 wt.% Huang (1998)
50 wt.% Jou (1993)
48.9 wt.% Jou (1982)
48.9 wt.% Austgen (1991)
Xu (1998)
50wt.% (this work 40 bar methane)
50wt.% (this work )
Figure 5 Literature data of the CO2-MDEA-H2O system at 313 K and 50 wt.%
MDEA
The figure shows that a lot of scatter exists in the literature data. The results of the
present experiments are in line with a large group of literature sources. However,
the data of Jou [10], [11] give CO2 partial pressures, which are substantially lower
than the other sources. This observation has also be seen at other conditions; data
by Jou show a lower CO2 partial pressure (higher CO2 solubility), which is also seen
in Figure 3. An explanation of this under-prediction of the acid gas partial pressure
might be that be that the MDEA used by Jou contained some impurities, such as
primary and secondary amines. These can have a large influence on the measured
170 Appendix A
acid gas solubility. However, the influence of amine impurities on the solubility
should vanish at higher liquid loadings and that is not seen in Figure 5, so the real
reason is not understood at this stage. The database used by Solbraa [26] for the
determination of the ionic interaction parameters of the CO2-MDEA-water system
was largely (approximately 35%) based on data by Jou; so a critical review of
available data has been carried out and new data have been included in the data
base. The following modifications to the original database of Solbraa [26] were
incorporated:
• All data of Jou [10], [11] have been omitted. As mentioned before these
data showed a systematically under-prediction of the acid gas partial
pressure;
• All data of Bhairi [3] have been omitted. These data showed a strange
behaviour at low loadings (no straight line of log-log graph of partial
pressure versus liquid loading);
• All data of Chakma [5] have been omitted, because of assumptions made in
the experimental procedure. The experiments of Chakma were carried out
at high temperatures (373-473 K) and no corrections for change in liquid
density and water evaporation were made. Also possible degradation of
MDEA at these high temperatures was not taken into account;
• Data of Rho [22] measured with 5 wt.% and 75 wt.% MDEA have been
omitted. These results cannot be validated and model simplifications, such
as neglecting CO32-
and OH- concentrations are not valid under these
conditions;
• Recent data of Kamps [13], Rogers [23] and Huang [9] were included. Low
loading data of Rogers [23] at 50 wt.% MDEA and 313 K were not used,
because these data were measured at very low loadings (< 0.004 mole CO2
/ mole amine) and at these conditions the model assumption that
concentration of OH--ions may be neglected is not correct.
An analysis of the quality of the solubility data of CO2 and H2S in MDEA available in
open literature is presented by Weiland [28]. In this work the experimental solubility
Appendix A 171
data (up to 1992) are compared with the Deshmukh-Mather thermodynamic model.
When experimental data deviate more than a factor 3 from the model result, the
data are qualified as not good. Compared with the database used in our work
Weiland concluded that 25% of the data of Jou [10] did not fulfill the criterium. In
contrast with this work, the data of Chakma [5] and Bhairi [3] were qualified as
good.
Incorporation of the above described modifications has resulted in the experimental
database in Table 5.
Ref. CMDEA
[wt.%]
Temperature
[K]
Liquid loading
[mole CO2 /mole
amine]
Data
points
[-]
Lemoine [17] 23.6 298 0.02-0.26 13
Austgen [2] 23.4 313 0.006-0.65 14
Kuranov [15] 19.2
18.8
32.1
313
313,333,373,413
313,333,373,393,413
1.56-2.46
0.36-2.62
0.41-4.46
9
32
40
Rho [22] 20.5
50
323,348,373
323,348,373
0.026-0.848
0.0087-0.385
32
26
Kamps [13] 32.0
48.8
313
313,353,393
0.85-1.24
0.12-1.15
5
23
Huang [9] 23
50
313,343,373,393
313,343,373,393
0.00334-1.34
0.00119-1.16
29
37
Rogers [23] 23
23
313
323
0.000591-.1177
0.001-0.07
14
6
Table 5 Literature references used for the fitting of the ionic parameters of the CO2
MDEA-H2O system
When the predictions of the original model of Solbraa [26] are compared with the
experimental data in Table 5, the BIAS and AAD are found to be 19.8 % and 26.7
172 Appendix A
ln lnx
BK A C T
T= + +
%. For this reason a new fit with the data base of Table 5 has been carried out to
get values for the ionic interaction parameters of MDEAH+-MDEA, MDEAH
+-H2O,
MDEAH+- CO2, and MDEAH
+-HCO3
-.
A.4.4 Influence of the MDEA dissociation constant (Ka)
In an aqueous MDEA solution with CO2 the following chemical reactions will occur:
1
2
3
4
2 3
2 2 3 3
2
2 3 3 3
2 3
2
2
K
K
K
K
H O H O OH
H O CO HCO H O
H O HCO CO H O
H O MDEAH H O MDEA
+ −
− +
− − +
+ +
⎯⎯→ +←⎯⎯
⎯⎯→+ +←⎯⎯
⎯⎯→+ +←⎯⎯
⎯⎯→+ +←⎯⎯
The equilibrium constants (based on mole fractions) of these reactions can be
correlated by the following equation:
Equation 2
The parameters for the equilibrium constants used by Solbraa [26] are given in
Table 6.
Kx A B C T [K] Reference
K1 132.899 -13445.9 -22.4773 273-498 Posey [26]
K2 231.465 -12092.1 -36.7816 273-498 Posey [26]
K3 216.049 -12431.7 -35.4819 273-498 Posey [26]
K4 -56.2 -4044.8 7.848 298-419 Posey [26]
Table 6 Parameters for calculation of the chemical equilibrium constants of the
system CO2-MDEA-H2O
The formation of carbonate-ions is usually limited, so reaction K3 is neglected. Also
the formation of OH- ions is neglected (reaction K1); this assumption may not be
Appendix A 173
2
1
MDEA
Ka
Kaγ
∞=
correct at very low liquid loadings. So, only reaction K2 and K4 are incorporated in
the E-EOS. The most important reaction is the protonation of MDEA to MDEAH+.
The fit of Posey [21] which was used by Solbraa [26] was based on experiments
carried out by Schwabe [24], Kim [14] and Oscarson [19]. In Figure 6 the pKa
measured by different authors is given as function of temperature and compared
with the fit of Posey [21]. For the fit of Posey a unit conversion from mole fraction to
molality has been incorporated.
6
6.5
7
7.5
8
8.5
9
270 290 310 330 350 370 390 410 430
Temperature [K]
pK
a [
mo
lality
]
Schwabe (1959)
Kim at al (1987)
Oscarson (1989)
Littel (1990)
Kamps (1996)
fit Posey (1997)
new fit
Figure 6 pKa of MDEA as function of temperature
The data measured by Schwabe [24], Kim [14], Oscarson [19], Littel [18] and
Kamps [12] presented in Figure 6 are at a reference state of infinite dilution for
MDEA. However, the data used in the work of Posey are based on a different
reference state: that of pure MDEA. The following relation is applicable between the
equilibrium constants at the two reference states of infinite dilution (Ka1) and pure
MDEA (Ka2):
Equation 3
174 Appendix A
Here ��MDEA is called the normalized activity coefficient. A new fit was prepared
using the literature data given in Figure 6, because in our model a reference state at
infinite dilution is used for all components except water. Only the data of Littel [18],
were not used, because these results were not in line with the other results. The
fitted equation was of the same type as the equations given by Posey [21] (refer to
Equation 2). The new fit results in the following fit parameters:
Kx A B C T [K]
K4 -77.262 -1116.5 10.06 278-423
Table 7 New fit parameters for the calculation of the MDEA dissociation constant
This equation is based on a reference state of infinite dilution. A conversion from the
molality scale (experiments) to the mole fraction scale (fit equation) has been
incorporated. Now the normalized activity coefficient as used by Posey can be
calculated and compared with the activity coefficient as calculated by the E-EOS. It
appears that these two activity coefficients do not match. At 313 K the two values
match very well, but at higher and lower temperatures, the deviations increase to
above 50 %. For this reason it was decided to use the new fit relation for the
dissociation of MDEA as described in Table 7. This new relation is then used in the
model with the reference state of infinite dilution. The new fit is shown in Figure 6.
With this new relation for the dissociation of MDEA, new ionic interaction
parameters of the system (CO2-MDEA-H2O) have been determined with the
modified database of Table 5.
A.4.5 Influence of the binary interaction parameters
With the new ionic interaction parameters a comparison between the changed
model results and the experimental data from Table 5 was carried out. The overall
BIAS and AAD deviations were 1.2 % and 23.8 %. When the model results were
compared it appeared that the fit with the higher concentration MDEA (50 wt.%) with
literature data was not good at lower liquid loadings.
Appendix A 175
There was a significant under-prediction of the partial pressure CO2 of the model. At
lower MDEA concentrations the fit of the model gave satisfactory results. A
comparison between model results and experimental data is presented for 50 wt.%
MDEA (Figure 7) and 23 wt.% MDEA (Figure 8).
1.0E-05
1.0E-04
1.0E-03
1.0E-02
1.0E-01
1.0E+00
1.0E+01
1.0E+02
1.0E+03
0.0001 0.001 0.01 0.1 1 10
Liquid loading [mole CO2/mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
50 wt% Rogers (1998)
50 wt.% Huang (1998)
48.9 wt.% Austgen (1991)
Xu (1998)
50wt.% (this work 40 bar methane)
50wt.% (this work )
simulation
Figure 7 Model results compared with experimental data for 50 wt.% MDEA
at 313 K
176 Appendix A
0.001
0.01
0.1
1
10
100
1000
0.001 0.01 0.1 1 10
Liquid loading [mole CO2/mole amine]
CO
2 p
art
ial
pre
ss
ure
[k
Pa
]
23 wt.% Huang (1998)
23.4 wt.% Austgen (1991)
23.4 wt.% Jou (1982)
20 wt.% @ 38 °C Bhairi (1984)
23.4 wt.% Mac. Gregor (1991)
Simulation
Figure 8 Model results compared with experimental data for 23 wt.% MDEA
at 313 K
When the physical solubility (solubility without reaction) of CO2 in the aqueous
MDEA solution calculated by the model is compared with experimental results
(using the CO2 - N2O analogy) the following graph was obtained.
Appendix A 177
2
2 2
2
,
, . , .
,
CO water
CO aq MDEA N O aq MDEA
N O water
HH H
H= ⋅
0
500
1000
1500
2000
2500
3000
3500
4000
0% 20% 40% 60% 80% 100%
Conc. aq. MDEA [wt.%]
H [
kP
a.m
3.k
mo
l-1]
model (298 K)
experiments (293 K) Pawlak (2002)
* experiments of Pawlak [20] have been converted from N2O to CO2 solubility using N2O-CO2 analogy
Figure 9 Physical solubility of CO2 in aqueous MDEA
Because CO2 reacts with MDEA, its physical solubility cannot be measured directly
and hence the CO2 - N2O analogy was used. This analogy is widely used in
literature and proven to be reliable for MDEA concentrations up to approximately
30wt.%. In view of the similarities of the configuration, molecular volume and
electronic structure N2O is often used as a non reacting gas to estimate the physical
properties of CO2 (Versteeg [27]). With this analogy the physical solubility (the
Henry constant H) for CO2 in aq. MDEA has been calculated in the following way:
Equation 4
178 Appendix A
From Figure 9 it can be seen that the estimation of the physical solubility in the E-
EOS contradicts to the experimental results. The model predicts a maximum in
solubility (minimum in H) as function of the MDEA concentration and the
experiments show a minimum solubility. The maximum error is seen at
approximately 50 wt.% MDEA. The physical solubility of CO2 in MDEA is mainly
determined by binary interaction parameters. Because no binary data are available
for the system CO2-MDEA, the interaction parameters were used as a fit parameter
in the ternary system (CO2-H2O-MDEA). So the calculated fit parameter from this fit
is probably in line with the data for the ternary ionic system, but does not agree with
the data from the binary system. A new approach to obtain a better value for this
interaction parameter has been proposed. The interaction parameters of the CO2-
MDEA system will be determined by fitting this value with the experimental data
available of the N2O solubility in aqueous MDEA and applying the N2O-CO2 analogy
to these data. This new approach has been included in Chapter 3 of this thesis.
A.5 Conclusions and recommendations
In the present Appendix new solubility data of CO2 and H2S in aqueous MDEA are
presented. Experiments have been carried out in a stirred reactor at elevated
pressures up to 69 bar (with methane as make-up gas). From these experiments it
is concluded that an increasing methane partial pressure results in a higher acid
gas partial pressure.
The results of the CO2 experiments are used to validate an electrolyte equation of
state (E-EOS). The E-EOS developed by Solbraa [26] has been improved in the
following aspects:
• The database used for the determination of ionic parameters for the CO2-
MDEA-H2O has been reviewed and modified;
• The equation for calculation of the dissociation of MDEA has been modified.
Instead of using the equation of Posey [21], which is based on a reference
Appendix A 179
state pure MDEA a new fit equation was developed based on a reference
state of infinite dilution.
The modified model is not able to estimate the CO2 partial pressure satisfactorily.
When the physical solubility of CO2 in aqueous MDEA is compared with
experimental data, a large deviation is observed. Most likely the binary interaction
parameter of CO2-MDEA, which is fitted using the reactive system of CO2-MDEA-
water is not correct. A new method is proposed to fit this parameter with the
experimental data of the N2O solubility in aqueous MDEA.
The results of the E-EOS look promising and the development will be continued.
However, as for every other model the input parameters are not known with
sufficient accuracy. The model is sensitive to the binary interaction parameters and
if they can not be determined accurately from data available in literature, additional
experiments will have to be carried out.
The following improvements to the electrolyte equation of state will be incorporated:
• Formation of carbonate will be included in the model. This reaction will
become important for high MDEA concentrations and/or high acid gas liquid
loadings;
• Formation of OH--ions will be included in the model. This reaction will
become important for low acid gas liquid loadings;
• A critical review of binary interaction coefficients will be carried out and
additional experiments done if not enough literature data are available;
• The model will be extended to predict the system H2S-MDEA-H2O-CH4;
• The model will be extended to predict the system H2S-CO2-MDEA-H2O-
CH4.
180 Appendix A
List of symbols
AR Residual Helmholtz Energy [J]
DEA Diethanolamine [-]
MDEA N-methyldiethanolamine [-]
MEA Monoethanolamine [-]
DMF Dimethylformamide [-]
TBAH TetrabutylammoniumHydroxide [-]
P (partial) Pressure [kPa]
AAD Absolute Average Deviation [%]
BIAS Mean BIAS Deviation [%]
K Chemical equilibrium constant [-]
H Henry’s coefficient [kPa.m3.kmole
-1]
Greek symbols
� Acid gas liquid loading [mole acid gas / mole
amine]
Activity coefficient [-]
Sub/super-scripts
i,j,I,n,x Index
exp Experiments
calc Calculated by model
� Infinite dilution in water
Aq Aqueous
Appendix A 181
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182 Appendix A
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Appendix A 183
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184 Appendix A
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185
List of publications
P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Gas solubility of
H2S and CO2 in aqueous solutions of N-methyldiethanolamine, Journal of Petroleum
Science and Engineering, 55 (2007) 122–134.
P.J.G. Huttenhuis, N.J. Agrawal, E. Solbraa, G.F. Versteeg, The solubility of carbon
dioxide in aqueous N-methyldiethanolamine solutions, Fluid Phase Equilibria, 264
(2008) 99-112.
P.J.G. Huttenhuis, N.J. Agrawal, G.F. Versteeg, The solubility of hydrogen sulfide in
aqueous N-methyldiethanolamine solutions, International Journal of Oil, Gas and
Coal Technology, 1 (2008) 399-424.
P.J.G. Huttenhuis, N.J. Agrawal, G.F. Versteeg, Solubility of carbon dioxide and
hydrogen sulfide in aqueous N-methyldiethanolamine solutions, Industrial &
Engineering Chemistry Research, 49 (2009) 4051-4059.
186 List of publications
Oral presentations
P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Experimental
determination of H2S and CO2 solubility data in aqueous alkanolamine solutions and
a comparison with an electrolyte equation of state, 1st Kuwait Oil and Gas
Conference and Exhibition, Kuwait, 7-9 March 2005.
P.J.G. Huttenhuis, N.J. Agrawal, J.A. Hogendoorn, G.F. Versteeg, Experimental
determination of H2S and CO2 solubility data in aqueous amine solutions and a
comparison with an electrolyte equation of state, Proceedings of the 7th World
Congress of Chemical Engineering, Glasgow, UK, 10-14 July 2005.
P.J.G. Huttenhuis, G.F. Versteeg, A comparison of different models for the
prediction of acid gas solubility in alkanolamine solutions, Proceedings of the 56th
Laurance Reid Gas Conditioning Conference, Norman, Oklahoma, 26 February – 1
March 2006.
187
Curriculum Vitae
Patrick Huttenhuis is geboren op 14 juni 1970 in Oldenzaal. Hij behaalde in 1988
zijn VWO diploma aan het Twents Carmel Lyceum te Oldenzaal. Hierna begon hij
met een studie Chemische Technologie aan de Hogeschool Enschede. In 1992
werd deze studie afgerond, nadat een afstudeeropdracht was uitgevoerd bij het
VEG-Gasinstituut te Apeldoorn. Van 1992 tot 1995 studeerde hij Chemische
Technologie aan de Universiteit Twente. Deze studie is afgerond in maart 1995,
nadat een afstudeeropdracht was uitgevoerd binnen de vakgroep proceskunde van
professor van Swaaij.
In 1995 begon Patrick zijn professionele carrière als process engineer bij het
ingenieursburo Stork Comprimo te Amsterdam (later overgenomen door Jacobs
Engineering). Binnen dit bedrijf was hij betrokken bij verschillende conceptual, basic
en detailed engineering projecten voor de chemische- en gasbehandelingsindustrie.
Deze projecten werden uitgevoerd op verschillende locaties in binnen- en
buitenland.
In 2002 is Patrick als senior process engineer in dienst getreden bij Procede Group
B.V. te Enschede. Binnen Procede heeft hij voornamelijk gewerkt aan
onderzoeksprojecten op het gebied van het verwijderen van zure gassen met
behulp van verschillende wasvloeistoffen. Als spin-off van een aantal van deze
projecten is dit proefschrift tot stand gekomen.
188 Curriculum Vitae
189
Dankwoord
Tenslotte ben ik aangekomen bij het laatste maar voor mij zeker niet
onbelangrijkste deel van dit proefschrift. Ik wil in dit hoofdstuk proberen duidelijk te
maken dat zonder de inzet van een heleboel anderen, ik dit proefschrift nooit had
kunnen schrijven. Het is niet mogelijk om in dit dankwoord iedereen te bedanken
die een bijdrage geleverd heeft, maar toch wil ik een poging wagen.
Als eerste wil ik mijn promotor Geert Versteeg bedanken voor het getoonde
vertrouwen in mij. Zijn enorme creativiteit, optimisme en kennis van “gas treating”
zijn voor mij altijd een bron van inspiratie geweest om stapje voor stapje dit
proefschrift af te kunnen ronden. Verder ben ik ontzettend blij met de bijdrage van
Neeraj Agrawal aan dit proefschrift. Ik leerde Neeraj kennen toen hij als TWAIO
begon aan zijn jaaropdracht. Na afronding van deze jaaropdracht trad Neeraj in
dienst bij Procede en is onze samenwerking verder voortgezet. Tijdens deze
periode zijn de meeste berekeningen met het thermodynamisch model uitgevoerd
door Neeraj. In 2005 is Neeraj begonnen aan een PhD studie aan de universiteit
van Pennsylvania, maar zelfs toen bleef hij erg betrokken bij mijn promotie project.
Tijdens deze periode werden nog verschillende berekeningen uitgevoerd en
commentaar geleverd op door mij geschreven wetenschappelijke artikelen. Neeraj,
thanks for your huge contribution to this project! Ook Even Solbraa heeft een zeer
belangrijke rol gespeeld binnen dit project. Even heeft de door hem ontwikkelde
code van het E-EOS model ter beschikking gesteld, maar ook een waardevolle
190 Dankwoord
bijdrage geleverd bij de verdere ontwikkeling van het model zoals beschreven in dit
proefschrift. Ook Sjaak van Loo wil ik van harte bedanken voor het gestelde
vertrouwen in mij en de mogelijkheid om mijn promotie in volledige vrijheid te
kunnen uitvoeren bij Procede. Ook de mogelijkheid om dit werk te kunnen
presenteren tijdens verschillende symposia in het buitenland was fantastisch. De
congressen die ik bezocht heb in Kuweit, Glasgow, Oaklahoma, Trondheim en
Frankfurt waren onvergetelijk. De mogelijkheid om een thermodynamica cursus aan
de universiteit van Kopenhagen (DTU) te volgen was ook geweldig. De bijdrage van
Kees Hogendoorn wil ik niet vergeten, omdat hij erg betrokken was bij het eerste
deel van dit proefschrift. Kees heeft mijn interesse gewekt in het bijzonder complexe
en interessante vakgebied van de “gas treating fundamentals”.
Ook het experimentele gedeelte van dit proefschrift is mede tot stand gekomen door
vele anderen. Als eerste wil ik alle collega’s bedanken die bij dit deel betrokken zijn
geweest: Henk ter Maat, Samuel Praveen, Piet IJben, Daniel Arslan en Eric
Wouters; bedankt voor jullie inzet. Verder wil ik uiteraard de technici bedanken die
betrokken zijn geweest bij de bouw van de opstellingen, die gebruikt zijn tijdens dit
project en niet minder belangrijk het operationeel houden van deze tijdens de
experimenten: Henk Jan Moed, Benno Knaken, Wim Leppink, Gerrit Schorfhaar en
Robert Meijer, hartelijk dank voor jullie inzet en enthousiasme; ook het kopje koffie
met jullie was altijd een vrolijk begin van de werkdag. Verder wil ik Wim Lengton
noemen die zeer betrokken is geweest bij de ontwikkeling van de vloeistof titraties
en Adri Hovestad voor de optimalisatie van de gasfase analyse met de gas
chromatograaf. Verder wil ik de Gas Processors Association bedanken voor de
financiering van het experimentele gedeelte van dit project.
De leden van de beoordelingscommissie, Ross Taylor, Erik Heeres en Hans
Wesselingh wil ik bedanken voor de beoordeling van dit proefschrift en het geven
van commentaar. Met name de zeer uitgebreidde bijdrage van Hans Wesselingh
heeft de leesbaarheid van dit proefschrift aanzienlijk verbeterd.
Dankwoord 191
Ik wil al mijn collega’s heel erg bedanken voor de prettige werksfeer en de leuke
tijd, die ik heb bij Procede. De talloze sportieve uitjes, zoals skiën, karten,
paintballen, wadlopen, schaatsen en niet te vergeten de etentjes en borrels waren
altijd erg gezellig. Mijn kamergenoot Peter Derks wil ik nog even apart noemen
vanwege de vele interessante gesprekken over voetbal, wielrennen, celebrities en
niet te vergeten “gas treating” even als Nick ten Asbroek, omdat hij op wil treden als
paranimf.
Ik wil al mijn vrienden bedanken voor de vele gezellige en sportieve activiteiten die
we regelmatig ondernemen en als het aan mij ligt zullen blijven ondernemen. Deze
activiteiten, waar ik altijd erg naar uitkijk zijn belangrijk en een hele goede
afwisseling met de dagelijkse bezigheden op het werk. Mijn speciale dank gaat uit
naar Harold Smelt; Harold, bedankt dat je wil optreden als paranimf.
Mijn ouders, zusjes en andere familieleden wil ik bedanken voor hun interesse en
steun in al mijn activiteiten. Tessa en Bas bedankt voor jullie altijd aanwezige
enthousiasme en interesse in mijn “boekje”. Vooral jullie lijfspreuk. “CO2 weg
ermee” gaf mij altijd de inspiratie en het relativeringsvermogen om dit werk af te
ronden. Tenslotte, wil ik Brigitte heel erg bedanken voor haar liefde, vertrouwen en
interesse. Ondanks dat ik haar niet heb vermoeid met de vele details van dit
onderzoek, kon ik altijd mijn verhaal kwijt en was zij een klankbord, waarmee ik voor
bepaalde problemen de juiste oplossingen kon vinden.
Patrick