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Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling Gas phase MCM development University of Leeds Department of Chemistry

Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

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University of Leeds Department of Chemistry. Gas phase MCM development. Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling. Overview. Update to MCMv3.1 Aromatic chemistry New schemes (MBO) Development of new schemes (MOST) Ethylene glycol di-vinyl ether (DVE-1) - PowerPoint PPT Presentation

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Page 1: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Gas phase MCM development

University of LeedsDepartment of Chemistry

Page 2: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Overview

Update to MCMv3.1

• Aromatic chemistry• New schemes (MBO)

Development of new schemes (MOST)

• Ethylene glycol di-vinyl ether (DVE-1)• Ethylene glycol mono-vinyl ether (MVE-1)• MOST EUPHORE 2005 photo-smog experiments

Future Work

• Update of photolysis rate parameters

Future scheme developments (open for discussion)

• UWA (Hong Kong/ Australian emissions) – Chloro-benzenes• Biogenics (Terpenes)• cyclohexanes/cycloalkenes

Page 3: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Development of MCMv3.1 - Aromatics

• Total aromatics form a significant fraction of anthropogenic VOC – from vehicle emissions and solvent use

• Highly reactive compounds with high emissions – substantial contribution to ozone formation

• Degradation schemes for 4 aromatics (benzene, toluene, p-xylene and 1,3,5-trimenthylbenzene) have been updated on the basis of new kinetic and mechanistic data

• Performance of these mechanisms evaluated using detailed photo smog chamber data from the EU EXACT campaigns

Heavily instrumented 200 m3 teflon foil chamber

Long path FTIR – aromatic parent compound, O3, HCHO, HNO3

UV absorption – O3 ; DOAS – NO2, glyoxal

Chemiluminescence – NO ; LIF – OH, HO2

Filter radiometer – J(NO2) GC techniques, HPLC, CO monitor

Page 4: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

• EXACT database contains photochemical smog chamber studies on all four mono-aromatics.

• Other experiments on specific key areas of aromatic oxidation, focusing on subsets of the toluene system.

• Where appropriate, results from EXACT have been used to refine the mechanisms.

• This development work on mono-aromatics has been extended to update the degradation schemes of the 12 other mono-aromatics with saturated alkyl side chains in MCMv3.1.

Development of MCMv3.1 - EXACT

Page 5: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

• Key areas in which the aromatic mechanisms have changed are:

Lower benzaldehyde yield in the toluene system.

Updated photolysis rates of unsaturated γ–dicarbonyls (ring opening products).

Breakdown of (5H)-furan-2-one (photolysis product of butenedial) has been updated and β–angelica lactone has been replaced by α–angelica lactone to reduce secondary glyoxal formation.

New phenol-type chemistry has been implemented reflecting lower yield for ring opening channel and need for reduced ozone formation from evaluation against EXACT/EUPHORE cresol smog chamber experiments.

Primary aromatic oxidation branching ratios have been adjusted to reflect new reported yields of glyoxal and phenol type compounds (under atmospheric conditions).

MCMv3.1 – Update of Aromatics

Page 6: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – Toluene Oxidation

OH

O

OO O O

O O

O O

OH

NO2O O

OH

O O

O O

O OO

O OO O

O

O

O

OH

25% 33%

PHENOL EPOXY PEROXY-BICYCLICRING-OPENING

22% 10%

95% 5%

H-ABSTRACTION

10%

1,4 - ADDITION

p-Methyl-benzoquinone

Benzaldehyde

4-oxo-2-pentenal Butenedial -Angelicalactone

(5H)-Furan-2-one

2,3-epoxy-6-oxo-4-heptenal

OH

O

OO O O

O O

O OO O

O OO

O OO O

OH

NO2

O O

OH

O O

OH

OH O

O

18% 65%

PHENOL EPOXY PEROXY-BICYCLICRING-OPENING

10% 7%

H-ABSTRACTION

7% 73% 20%

MCMv3

MCMv3.1

Page 7: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – EXACT Cresol Oxidation • Peak O3 is well simulated with MCMv3.1

• Representation of NO and NO2 profiles is improved

• However, radical yield is too low as rate of cresol oxidation is underestimated

• Results from comparison with EXACT cresol experiments used to adjust hydroxyarene degradation in MCMv3.1

• In MCM3.1a first generation ring retained products are treated in the same way as the original cresol

11 12 13 14 150

100

200

300

11 12 13 14 15

0

100

200

300

400

11 12 13 14 15

0

20

40

60

11 12 13 14 15

0

5

10

15

20

25

11 12 13 14 15-5.0x10

6

0.0

5.0x106

1.0x107

1.5x107

11 12 13 14 15

0.0

2.0x106

4.0x106

6.0x106

8.0x106

1.0x107

Cre

so

l [p

pb

]

Time [h]

Cresol (04/10/01)

experiment MCMv3 MCMv3.1 MCMv3.1a

O3 [

pp

b]

Time [h]

NO

2 [

pp

b]

Time [h]

NO

[p

pb

]

Time [h]

OH

[m

ole

cu

le c

m-3]

Time [h]

NO

3 [

mo

lecu

le c

m-3]

Time [h]

OH

OH

NO2

O O

OH

O O

OH

OHO

O

OH

OHOH

OH

OH

NO2

O O

OH

O O

OH

OH

OH

NO2

O O

NO2

OH

NO2

O2N

O O

OH

OH

O O

OH

O O

OH

O O

NO2

OH

O O

OH

O O

NO2

OH

O O

OH

O O

NO2

OH

O ONO2

7% 73% 20%

7% 7%73% 73% 20%20%

Page 8: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – EXACT Butenedial Oxidation

10 11 12 13 14 15

0

50

100

150

200

250

10 11 12 13 14 15

0

100

200

300

400

10 11 12 13 14 15

0

20

40

60

10 11 12 13 14 15

0

20

40

60

80

100

120

140

10 11 12 13 14 15

0.0

2.0x107

4.0x107

6.0x107

8.0x107

1.0x108

10 11 12 13 14 15

0

50

100

150

200

250

But

ened

ial[p

pb]

Time [h]

experiment MCMv3 MCMv3.1

O3

[ppb

]

Time [h]

NO

2 [p

pb]

Time [h]

NO

[ppb

]

Time [h]

OH

[mol

ecul

e cm

-3]

Time [h]

Butenedial (04/07/02)

HO

2 [p

pt]

Time [h]

• Faster removal due to increased photolysis rate in MCMv3.1

• However, OH and HO2 are much lower than measured

• NOxy chemistry poorly understood

• Secondary peak due to formation of PAN

• Ozone simulated well (coincidence?!)

Page 9: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – EXACT Benzene Oxidation

• O3 peak again greatly reduced using MCMv3.1

• Good agreement due to increase in phenol yield

• However, increase in ring-retaining products leads to a decrease in oxidising capacity of the system (OH better simulated using MCMv3)

• This is indicative of the general mechanistic problem:

Over prediction of O3 but under prediction of the

system reactivity.

10 11 12 13 14 15 16 17

1200

1400

1600

1800

2000

10 11 12 13 14 15 16 17

0

50

100

150

200

250

300

10 11 12 13 14 15 16 17

0

5

10

15

20

25

30

35

10 11 12 13 14 15 16 17

0

10

20

30

40

50

Ben

zene

[ppb

]

Time [h]

Benzene, low NOx (08/07/02)

experiment MCMv3 MCMv3.1

O3 [p

pb]

Time [h]

NO

2 [pp

b]

Time [h]

NO

[ppb

]

Time [h]

Page 10: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – EXACT Toluene Oxidation

• O3 peak still greatly overestimated using MCMv3.1

• increased branching for ring open products (early)

• increased photolysis of unsat. dicarbonyls (early)

• changes in phenol chemistry decreases O3 formation in middle of experiment

• higher “missing” OH for MCMv3.1

• Reduced oxidative capacity consistent with reduced O3 formation potential

10 11 12 13 14 15 16

200

400

600

10 12 14 16

0

200

400

10 11 12 13 14 15 16

0

20

40

60

80

100

10 11 12 13 14 15 16

0

50

100

150

Tol

uene

[ppb

]

Time [h]

experiment MCMv3 MCMv3.1

O3 [p

pb]

Time [h]

Toluene, moderate NOx (27/09/01)

NO

2 [pp

b]

Time [h]

NO

[ppb

]

Time [h]

Page 11: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – Update of Aromatics

• In general MCMv3.1 shows improved ability to simulate some of the EXACT observations and represents our current understanding of aromatic degradation.

• However, significant discrepancies remain concerning ozone formation potential and oxidative capacity of aromatic hydrocarbon systems:

Peak O3 is simulated well for benzene but over estimated for the substituted aromatics. OH radical production is too low to account for the OH inferred from the rate of loss of the parent aromatic. For a majority of the systems the NO oxidation rate is under predicted. This parameter is linked to the production of O3 and the oxidative capacity of the system.

• Ideas and strategies for resolving these issues have been suggested and additional laboratory and smog chamber experiments are required in order to investigate them further.

Page 12: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MCMv3.1 – Other updates

• New scheme for biogenic hydrocarbon MBO (2-methyl-3-buten-2-ol) added with 93 new reactions, 30 new species

OH

OH

OOH O

O OH

OO OO2N

OC

OH

O O

OH

O

CH2 O O

+ OH

0.67 0.33 0.65 0.35

+NO3 + O3

0.70.3

HCHO

HO2HCHO HO2

HO2

HCHO NO2

MBO

All major new products already in MCM

• Extended list of chloro- and hydrochlorocarbons and 2 hydrobromocarbons

• MCMv3.1 now contains 135 primary emitted VOCs

c.a. 5600 species and 13500 reactions

Page 13: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Mechanism Development – MOST

Multiphase chemistry of Oxygenated Species in the Troposphere

Page 14: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Mechanism Development – MOST

Multiphase chemistry of Oxygenated Species in the Troposphere

• Organic solvents are used in a large number of industrial processes and due to their volatility many are emitted either directly or indirectly into the atmosphere.

• A number of organic compounds employed as solvents at the present time have been shown to have adverse health effects, carcinogenic, mutagenic and reprotoxic properties

• Solvents also undergo complex chemical reactions in the atmosphere, which lead to the formation of compounds which are environmentally damaging, in particular the formation of photochemical oxidants

• It is now well accepted that the switch from additional solvents to oxygenated compounds is inevitable both in terms of toxicity problems and in order to reduce the levels of oxidant formation in the troposphere

• The solvent industry within Europe has targeted a limited range of ethers, ketones, esters and glycols as replacements for traditional solvents

Page 15: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MOST – Key Oxygenates

O

O

N O

O

O

OO

OH

O

O

OO

O

OO

OO

OO

OH

MEK

MIBK

ODVE

DDVE

MVE-2

CHDVE

DVE-2

DVE-3

NMP

DPM

In McM

Page 16: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MOST EUPHORE 2005 - Proposal

“To Carry out carefully designed chamber experiments involving the measurement of reactants, intermediates and products in the

presence of NOx under conditions which simulate ambient tropospheric conditions (NOx and VOC limited)”

(c.f. EXACT 2001-2002)

These experiments will build upon/bring together what we have learned from the MOST chamber studies 2002/2003

Page 17: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

OO

MOST EUPHORE 2005 – Model Compounds

• Experiments to be carried out with model compounds

short chain to suppress isomerisation symmetrical known products (easy to calibrate, can we measure them easily?) simplify chemistry separate experiment(s) focussing on important intermediates

(eg. formates)?

• Chosen models: DVE-1 • (Ethylene glycol di-vinyl ether)• Vinyl ether model• Aerosol formation (OH and O3)

MVE-1• (Ethylene glycol mono-vinyl ether)• Vinyl alcohol model• Aerosol formation (OH and O3)

OOH

Page 18: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Explicit mechanism construction

Approaches:

• Construction “by hand” following MCM protocol.

• MECHGEN automatic generation using expert systems techniques used as an initialisation tool.

Problems:

• MECHGEN does not allow for use of experimental values, only SARs are used.

• Implemented SARs/GRs may not be appropriate for these oxygenated species.SARs: Kwok and Atkinson, Atmos. Env., 29, 1685 (1995).

Peeters et al., Chemosphere, 38, 1189, (1999).

GR: Porter et al., J. Phys. Chem. A., 101, 5770 (1997).

Page 19: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Mechanistic Detail – DVE-1 + OH

• Rate constant estimated by analogy

OO

OO

DVE-1CH2=CHOCH2CH2OCH=CH2

Similar reactivity to ether equivalent CH3OCH2CH2OCH3

2.7 × 10-11cm3 molecule-1 s-1

(from Mellouki et al [2004])

O

O

O

Mono-vinyl ether k298 (cm3 molecule-1 s-1)

Methyl vinyl etherMVE

ABSa N/ARRb 4.5 × 10-11

Ethyl vinyl etherEVE

ABSa 6.8 × 10-11

RRb 7.2 × 10-11

AVERAGE 7.0 × 10-11

Propyl vinyl etherPVE

ABSa 1.0 × 10-10

RRb 1.05 × 10-10

AVERAGE 1.025 × 10-10

Technique Reference Estimated kOH (298, cm-3 molecule-1 s-1)

Analogy (see above) 16.7 × 10-11

Group Reactivity (GR) Porter et al. (1997)Peeters et al. (1996)

8.52 × 10-11

Structure Activity (SAR) Kwok and Atkinson (1995) 8.77 × 10-11

Page 20: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

DVE-1– degradation scheme 1 (OH)

OO

OHO

O

OO

OO

O

OO

OO

OO

O

OHO

O

OO

O

OO

O

O

OO

OO

O

OO

O

O

OO

OOO

OO

OO

OHO

O

OO

O

OO

O

O

DVE-1

NO2

HO2

+ HCHO

(2*0.053)+(2*0.352) = 0.81

OH Add OH Abs

OH Add

0.095+0.095 = 0.19

DVE1FM

NO2

HO2

DVE1CONE

NO2

HO2

ETHDFM

+ HCHO

NO2

HO2

DVE1CKFM

NO2

HO2

C5O4FMB

OH Abs

OH Abs0.68 0.16

0.16

NO2

HO2

DVE1CKFM

+ HCHO

OH Add

332 OH initiated reactions kOH = 8.77E-11 (SAR)

= 8.52E-11 (GR)

= 16.7E-11 (AN)

Page 21: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

DVE-1– degradation scheme 2 (OH)

OO

OO

O

OO

O

O

OO

O

O

OO

OO

O

O O

OO

O O

O

O

O O

OO

O O

O

O

O O

O

O

O

OO

O

O

O

O

O

O O

O

O OO

O O

O

O OO

DVE-1

NO2

HO2

+ HCHO

(2*0.053)+(2*0.352) = 0.81

OH Add OH Abs

OH Add

0.095+0.095 = 0.19

DVE1FM

NO2

NO2

HO2

ETHDFM

+ HCHO

DVE1CKFM

NO2

HO2

C5O4FMB

OH Abs

OH Abs

0.68

0.16

0.16

NO2

HO2

NO2

HO2

OH Abs

NO2

HO2

OH Add

+CHOOCHO

NO2

HO2

OH Abs

NO2

HO2

OH Add

C2DOCHO

+ HCHO

NO2

HO2

OH Abs

+CHOOCHO

CO

NO2

HO2

OH Add

C2DOCHO

+ HCHO

NO2

HO2

OH Abs

+CHOOCHO

CO

NO2

HO2

OH Abs0.14

0.86

+ CO

CCOCHO

+

CCOCHO

CCOCHO

HCHO

NO2

HO2

NO2

HO2

OH Add

+CHOOCHO

HCHO

NO2

HO2

OH Add

+CHOOCHO

HCHO

+CHOOCHO

HCHO

Page 22: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Mechanistic Detail – DVE-1 + O3

• Rate constant estimated by analogy

O

O

Mono-vinyl ether k298 (cm3 molecule-1 s-1)

Ethyl vinyl etherEVE

2.0 × 10-16

Propyl vinyl etherPVE

2.4 × 10-16

• Rate constant measured on 27/5/04 at EUPHORE:

kDVE-1+O3 = [2((2.0 + 2.4)/2)] × 10-16 = 4.4 × 10-16 cm3 molecule-1 s-1

kDVE-1+O3 = 2.5 (± 0.3) × 10-16 cm3 molecule-1 s-1

Page 23: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

DVE-1– degradation scheme 1 (O3)

OO

OO

O

OO

O OOO

OO

OO

OH

H

OO OH

O

OO

O OOO

OO

O

OO

OO

DVE-1

*

0.50.5

*+ HCHO +

*

CCOCCHO

+ CO

+ OH+ CO2

HO2

+ CO2

HO2

HO2

0.24 0.20

0.36 0.20

CO

NO

SO2

NO2

H2 O

DVE1FM

DVE1FMMVE-1

CCOCCHO

O3

Page 24: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

DVE-1– degradation scheme 2 (O3)

OO

O

OO

O

O OOO

O

OO

O

O

OOH

H

OO

O

OHO

O

OO

O

OO

O

OO

O

O

O OOO

O

OO

O

OO

O

OO

O O

OO

O O

O

O

O

O

O O

DVE1FM

*

0.50.5

*

+ HCHO+

*

+ CO

+ OH

+ CO2

HO2

+ CO2

HO2

HO2

0.24 0.20

0.36 0.20

CO

NO

SO2

NO2

H2O

C2DOCHO

O3

O3

ETHDFM

MOXY2CHO

O3

ETHDFMETOHOCHO

MOXY2CHO

C5O4FMB

CCOCHO CHOOCHO

Page 25: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MVE-1– degradation scheme (OH)

kOH = 1.03E-10 (RR) latest

= 1.20E-10 (RR)

= 6.4E-11 (RR)

= 4.67E-11 (GR)

= 4.80E-11 (SAR)

319 reactions including OH, O3 and NO3

OOH

OHO

OH

OO

OO

OH

OHO

OOH

OO

OOH

OOH

O

OOH

O

O

O OO

OOH

O OO

O

O O

OO

OH

OO

OO

O

O OO

O

O

MVE-1

NO2

HO2

+ HCHO

ETOHOCHO

NO2

HO2

+ HCHO

ETOHOCHO

NO2

HO2

+ HCHO

HO2

0.640.096 0.156

0.105

OH AddOH Add

OH AbsOH Abs

OH Add

NO2

HO2

+CHOOCHO

HCHO

OH Add

NO2

HO2

MOXY2CHO

+ HCHO

j 15

HO2

+ CO

NO2

HO2

Products

HCHO (100%)

ETOHOCHO?

Page 26: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

MVE-1– degradation scheme (O3)

OOH

OO

O

OOH

O OOHO

O

OH

O

OOH

H

O OOHO

OOH

OHOH

OOH

OOH

OOH

OOH

O

OO

O

O

O O

OO

O

O

MVE-1

*

0.50.5

*+ HCHO +

ETOHOCHO

*

HOCH2CH2O

+ CO

+ OH+ CO2

ETHGLY

HO2

HOCH2CH2O

+ CO2

HO2

HOCH2CHO

HO2

HOCH2CHO

0.24 0.20

0.36 0.20

CO

NO

SO2

NO2

H2 O

ETOHOCHO

MOXY2CHO

CHOOCHO

O3

O3

kO3 = 1.8 (± 0.7) E-16 latest

Page 27: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Isopleth Plots

Maximum O3 formation as a function of initial NO and VOC concentrations in simulated chamber experiments.

• Identify initial conditions for VOC limited and NOx limited regimes.

• Used to choose conditions for chamber experiments on aromatic compounds (EXACT).

130

260

390 520

650

780910

10401170

13001430

1560 1690

1820

1950 2080

2210

2340

130200 400 600 800 1000 1200 1400 1600 1800 2000

200

400

600

800

1000

1200

1400

1600

1800

2000

NO

/ pp

bv

DVE1/ ppbv

Page 28: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Future Work

Update of Photolysis Reactions

Page 29: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Update of Photolysis Reactions (1)

• Photolysis rates for a core number of reactions (as a function of SZA) have been determined using a two stream isotropic scattering model (on 1st July at 0.5 km, lat. 45oN).

• Variation of j with SZA is described well by the following expression:

j = l (cosX)mexp(-n.secX)

• Some of these parameters are then used to define the photolysis rate of a large number of related species.

• However, the laboratory measured cross sections and quantum yields for these core reactions have not been updated since 1997 and new measurements have also have become available.

Page 30: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Update of Photolysis Reactions (2)

Page 31: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Update of Photolysis Reactions (3)

1.00E-03

1.50E-03

2.00E-03

2.50E-03

3.00E-03

3.50E-03

4.00E-03

0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4

SZA/ Radians

j-v

alu

e/ s

-1

HCHO_R/NO2 MCM

HCHO_R/NO2 TUV4.2

0.00E+00

4.00E-04

8.00E-04

1.20E-03

1.60E-03

2.00E-03

0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4

SZA/ radians

j-v

alu

e/ s

-1

nC3H7CHO/NO2 MCM

HOCH2CHO/NO2 TUV4.2j-(HOCH2CHO) chamber

cs – Atkinson et al. (2002)qy – Atkinson et al. (2002)

j-(n-C3H7CHO) (j<15>) MCM

cs – Roberts and Fajer (1989)qy – Atkinson et al. (1992)

j-(HCHO_R) chamber

cs – Atkinson et al. (2002)qy – Atkinson et al. (2002)

j-(HCHO_R) (j<15>) MCM

cs – DeMore et al. (1994)qy – DeMore et al. (1994)

Page 32: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Update of Photolysis Reactions (4)

• MCM photolysis rate parameters need to be recalculated using up to date spectroscopic and photochemical information.

• A thorough literature review is currently underway

• New calculations will be carried out using the discrete ordinate

radiative transfer models TUV (www.acd.ucar.edu/TUV) and PHOTOL (Jenkin et al. 1997b).

Page 33: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Future Work

New Reaction Schemes

Page 34: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Future Scheme Development

What to do next?

• Biogenics – Terpenes (sequiterpenes)

• Cyclohexanes

• Cycloalkenes

• Chloro-benzenes (Hong Kong and China emissions)

Page 35: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Cyclohexanes: NAEI Speciationcyclohexane 2.579 cyclopentane 0.181propylcyclohexane 2.473 1,2-dimethyl-3-isopropylcyclopentane 0.178c10-cyclo-paraffin 2.249 (2-methylbutyl)cyclohexane 0.154(1-methylpropyl)cyclohexane 2.072 c11-cyclo-paraffin 0.1541-methyl-4-isopropylcyclohexane 2.002 dimethylcyclohexane 0.148butylcyclohexane 1.901 cycloheptane 0.1301-ethyl-3-methylcyclohexane 1.716 c9-cyclo-paraffin 0.124methylcyclohexane 1.423 ethylcyclopentane 0.123methylcyclopentane 1.399 1,2-dimethylcyclopentane 0.122(1-methylethyl)cyclohexane 1.152 1,3-dimethylcyclopentane 0.122(2-methylpropyl)cyclohexane 1.128 methylcyclodecane 0.1011,2,3-trimethylcyclohexane 0.981 1,2,4,4-tetramethylcyclopentane 0.0862,2,3,3-tetramethylhexane 0.758 cyclo-paraffin 0.0771-ethyl-4-methylcyclohexane 0.734 c12-cyclo-paraffin 0.069ethylcyclohexane 0.700 1,1-dimethylcyclohexane 0.0391-ethyl-2,2,6-trimethylcyclohexane 0.580 1,2-ethylmethylcyclopentane 0.0391,4-dimethylcyclohexane 0.574 trimethylcyclopentanes 0.0361,1,3-trimethylcyclohexane 0.533 1,2,3-trimethylcyclopentane 0.0351,2,3,5-tetramethylcyclohexane 0.525 dimethylcyclohexanes 0.0351,1,2-trimethylcyclohexane 0.464 methyltetralin 0.032pentylcyclohexane 0.464 propylcyclopentane 0.028decalin 0.406 1,2,4-trimethylcyclopentane 0.019tetramethylcyclohexane 0.371 1-ethyl-2-methylcyclopentane 0.019octahydro-indan 0.341 1-ethyl-3-methylcyclopentane 0.019C-7 CYCLOPARAFFINS 0.341 cyclooctane 0.0191,1,4,4-tetramethylcyclohexane 0.332 isopropylcyclopentane 0.0191,2,4-trimethylcyclohexane 0.302 methylcycloheptane 0.0191-methyl-1-propylcyclopentane 0.293 trimethylcyclohexanes 0.0171-ethyl-2,3-dimethylcyclohexane 0.263 1,3-ethylmethylcyclopentane 0.0161,2-dimethylcyclohexane 0.259 1,2,4-trimethlycyclopentane 0.009decalin(trans) 0.251 1-methyl-3-isopropylcyclopentane 0.0091,3-dimethylcyclohexane 0.242 hexylcyclohexane 0.0091-ethyl-2-propylcyclohexane 0.240 tertbutylcyclopropane 0.0091-ethyl-1,4-dimethylcyclohexane 0.231 propylcyclohexanes 0.005dimethylcyclopentanes 0.205 butylcyclohexanes 0.003

Page 36: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Building a Hong Kong (HK) Photochemical model

Page 37: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Hong Kong Data Set• Air monitoring network data available for > 5 years,

includes standard MET, NOx, Ozone, CO, SO2, TEOM PM10 and PM2.5, VOC (>200)

• Beginning analysis of datasets to characterise air masses for high pollutant events e.g. measured O3 on 9th June 2004 in excess of 200 ppb

• Identify significant VOC currently not included in the MCM, to enable construction of a HK photochemical model

• Work initiated 1 Dec 2004, with masters student from HK Polytechnic University

Page 38: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Hong Kong Data Set• Emissions and monitoring

Page 39: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Identified missing VOC species• Current MCM species• 135 VOC

• HK Monitoring data> 100 compounds

• 18 halo-compounds• 10 aromatic• 9 halo-aromatic• 38 HC’s (mostly higher alkanes, alkenes, cyclo-alkanes and cyclo-alkenes)• 2 carbonyl compounds

Page 40: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Suggested VOC for expansion of MCM

• New project initiatives require VOC scheme expansion

• Some expansion work begun– Chlorobenzene– 1,5-pentanedial

• Other species identified– Key VOC for HK model work– Biogenics; 1,8-cineole, d-limonene– DMS, DMDS

Page 41: Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling

Some possible candidates identified from various emissions inventories

• Alkylcyclohexanes• 3-heptanone• Ethyl hexanal• Other chlorobenzenes• 1-methyl 4-isopropyl benzene• 3-methylbenzaldehyde• Propyne• Acrolein, vinyl acetate, crotonaldehyde – to be further

expanded as primary VOC (currently secondary species)