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Accurate elemental speciation by
isotope dilution mass spectrometry with hyphenated techniques
Klaus G. Heumann Institute of Inorganic Chemistry and Analytical Chemistry
Johannes Gutenberg-University Mainz, Germany
Important limitations of hyphenated techniques
These techniques do not prevent and identify possible species transformations during the different analytical steps
Accurate quantification is often not an easy task due to matrix effects, system instabilities etc.
Lack of adequate validation methods
Validation of speciation analysis methods
Difference between precision (statistical error) and accuracy (inaccurate values
are related to systematical errors)
Artifact formation of MeHg in sediments (March 1999)
Concern over possible formation of MeHg artifacts during certain analytical procedures was first expressed at the „1996 Mercury as a Global Pollutant“ conference. Many laboratories now doubt that the CRMs they use are indeed properly certified. The findings on artifact formation are not sufficient to claim that MeHg results are overestimated.
Methyl mercury revisited (September 1999)
Recently, some of our European colleagues involved in the production and certification of environmental reference materials have declared that the potential for artifact MeHg formation during analysis is of little concern. We strongly disagree with this stance, because it undermines the scientist`s obligation to strive for the greatest accuracy possible.
A series of letters to the Editor of the journal ‚Analytical Chemistry‘ were sent in 1999
Who is correct ? Can this be solved by letters to an analytical journal or
should it be better solved by isotope dilution mass spectrometry ?
NS = NSp (hSp2 - R x hSp
1) / (R x hS1 - hS
2)
R isotope ratio (only data to be measured)
NS, Sp number of sample and spike atoms
h1,2 isotope abundance of reference and spike isotope
Isotope 1 Isotope 2
Sample Isotope diluted
sample Spike
Inte
nsity
Isotope 1 Isotope 2 Isotope 1 Isotope 2
The principle of isotope dilution mass spectrometry (IDMS)
Only the isotope ratio of the isotope diluted sample must be measured – and not an absolute amount of the analyte !
Isotope ratio measurement is independent on:
Matrix effects
Signal drifts of the instrument
Sample loss does not affect the result after the isotope dilution step has taken place (determination of recovery not necessary)
Experimental conditions for IDMS
However, detection methods with multi-element capability like ICP-MS have a high risk of wrong results by spectrometric interferences
The species-specific spiking mode
Elemental species must be well defined by composition and structure, e.g. CrO4
2-, IO3-, MeHg+ ……
Best spiking mode if isotope-labeled species is available (spiking prior to separation)
Isotope-labeled species must usually be synthesized
The isotopic composition is constant over the whole chromatographic peak (real-time determination)
Isotope exchange between different species must be avoided
How complicated is synthesis of isotope-labeled species ?
Relatively simple for most inorganic species like iodate:
Na129I Na129IO3
Not too complicated for organometallic species like MeHg+:
Usually too complicated or impossible for large biomolecules
201HgCl2 + Me-Co Me201Hg+
Me-Co = Methylcobalamin
HNO3/HClO3
Determination of inorganic iodine species in a mineral water sample determined by species-specific IC/ICP-IDMS
Spike: 129I- and 129IO3-
3.13 ng I/mL
0.30 ng I/mL
Sum of species analysis 3.43 ng I/mL Total I by ICP-IDMS 3.44 ng I/mL
Commercially available spike compounds
Institute for Reference Materials and Measurements (IRMM), Geel/Belgium:
Isotopically labeled 202HgMe+ spike
ISC Science, Gijón/Spain:
119SnBu3+ / 119SnBu22+ / 119SnBu3
+ (mixed spike)
Chromatogram of a multi-species determination by species-specific GC/ICP-IDMS (mussel tissue, CRM 477)
(N. Poperechna and K.G. Heumann)
20
0 Hg
/ 208 P
b
0 2 4 6 8 1 0 1 2
0
1 0 0 0
2 0 0 0
3 0 0 0
4 0 0 0
Bu3
Sn+
Bu2
Sn2+
BuS
n3+
Me3
Pb+
MeH
g+
0
5 0 0 0
1 0 0 0 0
1 5 0 0 0
2 0 0 0 0
0 2 4 6 8 1 0 1 2
0
1 0 0 0
2 0 0 0
3 0 0 0
4 0 0 0
0
5 0 0 0
1 0 0 0 0
1 5 0 0 0
2 0 0 0 0Bu3
Sn+
Bu2
Sn2+
BuS
n3+
Me3
Pb+
MeH
g+
202 H
g / 20
6 Pb
1
19Sn
12
0 Sn
Retention time (min)
Reference isotopes
Spike isotopes
0
4000
2000
4000
2000
0
Inte
nsity
(cp
s)
20000
10000
0
20000
10000
0
Results of multi-species determination by species-specific GC/ICP-IDMS in mussel tissue (CRM 477) and tuna fish (CRM 463)
Species CRM 477 CRM 463
GC-ICP-IDMS Certified GC-ICP-IDMS Certified
Me3Pb+ (ng/g) 0.34 ± 0.03 0.30 ± 0.02 * 4.10 ± 0.16 4.39 ± 0.16 *
MeHg+ (µg/g) 0.066 ± 0.02 --- 2.95 ± 0.05 2.83 ± 0.15
BuSn3+ (µg/g) 0.93 ± 0.04 1.01 ± 0.19 < 0.0003 ---
Bu2Sn2+ (µg/g) 0.82 ± 0.03 0.78 ± 0.06 < 0.0012 ---
Bu3Sn+ (µg/g) 0.85 ± 0.01 0.90 ± 0.08 < 0.0003 ---
* Indicative value
Excellent agreement between GC-ICP-IDMS and certified/indicative values
The species-unspecific spiking mode
Necessary for all elemental species where exact composition and structure is not known, e.g. metal complexes of humic substances, proteins …..
Addition of spike must be carried out after complete separation of species
Spike may exist in any chemical form
The isotope ratio varies over the whole chromatographic peak (however, real-time concentrations are available)
Signal intensity of the measured element must be independent on the species form (found for normal nebulizer systems like cross-flow, but not for ultrasonic nebulizer with membrane desolvator)
Conversion of an isotope ratio chromatogram for a copper species into a mass flow chromatogram
6
8
10
12
14
0 10 20 30Retention time [min]
65C
u/63
Cu
ratio
spike isotope ratio
Isotope ratio chromatogram
0
1
2
3
4
5
0 10 20 30Retention time [min]
Mas
s flo
w C
u [p
g/s]
Mass flow chromatogram
Distribution of heavy metals in SEC separated fractions of two different waste water samples from a sewage disposal plant by HPLC/ICP-IDMS
In both waste water samples the distribution of different heavy metals is different
Zn prefers a high molecular fraction, Cu interacts with most fractions and Mo only with a small fraction of medium molecular weight
For volatile elemental species
GC/ICP-IDMS
can be used in the species-specific and
species-unspecific spiking mode
Hg0 Hg2+
MeHg+ Me2Hg
Example: Determination of monomethylmercury MeHg+ by
species-specific GC/ICP-IDMS
Hg in environmental samples is present in different species
Air
Biomethylation by algae and bacteria
Soil and rocks
He AFS
AES
drying tube
valve
alkylation and purging vessel
cold trap
+ -
atom emission detector
heating unit
capillary GC
ICP-MS
oven atom fluorescence detector
inductively coupled plasma MS
MeHg+ + NaBEt4 MeEtHg
Hg2+ + NaBEt4 Et2Hg
Ethylation of mercury species by NaBEt4:
Hyphenated GC/atom spectrometric techniques for determination of MeHg+ in water samples
0
40
80
120
160
0 2 4 6 8Retention time [min]
Inte
nsity
[x 1
03 cp
s] 201202
75
90
105
120In
tens
ity [m
V]
GC/ICP-MS:
GC/AFS:
• Quantification usually by external calibration
• Application of IDMS possible
• Additional information on isotope ratios
• 201Hg/202Hg = 0.44 for all species
Gas chromatogram of a mercury species standard solution detected by AFS and ICP-MS
Hgo MeHg+ Hg2+
Spike isotope ratio 201Hg/202Hg = 6.53 (natural = 0.44)
0
40
80
120
0 2 4 6 8Retention time (min)
Inte
nsity
(x 1
03 c
ps) 201
202Me201Hg+
Characterization of a Me201Hg+ spike solution by GC/ICP-MS
A species-pure monomethylmercury spike was obtained
0
50
100
150
200
0 2 4 6 8Retention time (min)
Inte
nsity
(x10
3 cp
s)201202
Hg0 201Hg/202Hg=1.65
MeHg+ 201Hg/202Hg=4.45
Hg2+ 201Hg/202Hg=0.44
MeHg+ analysis in seawater by GC/ICP-IDMS using a Me201Hg+ spike
Transformation of MeHg+ into Hgo
Transformation can only be identified by isotope-labelled species
Determination of MeHg+ in a river water sample spiked with Me201Hg+ prior to alkylation by NaBEt4 and NaBPr4
Inte
nsity
(10
3 cps
)
201202
0
50
100
150
200
250 201202
0 2 4 6 8 10 0 2 4 6 8 10
Retention time (min)
Ethylation Propylation
201Hg/202Hg = 1.69
MeHg+ = 3.8±0.1 pg/mL
Hgo
Hg2+
201Hg/202Hg = 1.61
MeHg+ = 3.6±0.1 pg/mL
Hgo
Species transformation by ethylation but not by propylation
However, in both cases identical results are obtained !
What can we learn from species-specific GC/ICP-IDMS of methylmercury ?
The use of isotope-labeled species identifies species transformations
Even if species transformation takes place, accurate quantification is possible by species-specific GC/ICP-IDMS
(if total mixture between sample and spike species has taken place prior to transformation)
Species-specific ICP-IDMS can best be used for validation of analytical methods for elemental species !
Certified value: (70.3 ± 3.4) ng g-1
GC/ICP-IDMS: (72.6 ± 1.3) ng g-1
Certified value: (2.83 ± 0.15) µg g-1
GC/ICP-IDMS: (2.91 ± 0.07) µg g-1
CRM 580 (sediment) CRM 463 (tuna fish)
Sediment sample + Me201Hg+ in diluted HNO3
Biolog. sample + Me201Hg+ in TMAH
Buffering at pH 4.8 and ethylation by NaBEt4
In-situ extraction of MeEtHg by nonane (5 min)
Microwave extraction (5 min)
Injection of nonane extract into GC 201Hg/202Hg isotope ratio measurement in separated mercury species (6 min)
Determination of MeHg+ in environmental and biological samples by species-specific GC/ICP-IDMS
Isotope exchange between different species must be avoided
Is this precondition always fulfilled ?
Example:
Determination of volatile halogenated hydrocarbons by GC/ICP-IDMS
Iodine isotope chromatogram by GC/ICP-MS of an 129I-labeled ethyl iodide spike
A species-pure ethyl iodide spike was obtained
129I-labeled iodide solution
Addition of NaBEt4 in MQ-water
Addition of acetate buffer
Extraction by nonane 0
2000
4000
6000
8000
10 15 20 25
129I
127I
C2H5I
Retention time (min)
129I/127I = 5.4
Inte
nsity
(cps
)
Retention time (min)
Iodine isotope chromatogram by GC/ICP-MS of natural iodinated hydrocarbons spiked with 129I-labeled ethyl iodide
0
2000
4000
6000
5 10 15 20 25 30
CH
3I
C2H
5I
2-C
3H7I
1-C
3H7I
CH
2ClI
129I
127I
CH
2I 2
Isotope exchange takes place with all iodinated species
Species-specific IDMS not possible !
81Br and 79Br chromatograms of a 79Br-labeled ethyl bromide spike
Species-pure 79Br-labeled C2H5Br spike could be synthesized by ethyl tosylate:
NH479Br + C2H5Ts C2H5
79Br + NH4Ts
0 5 10 15 20 25 30 35 0
2000
4000
6000
8000
10000
12000
79 B
r Int
ensi
ty (c
ps)
Retention time (min)
79 Br chromatogram
0
2000
4000
6000
8000
10000
12000
81 B
r Int
ensi
ty (c
ps)
81 B r chromatogram
81Br and 79Br chromatograms of natural brominated hydrocarbons spiked with 79Br-labeled ethyl bromide
No isotope exchange occurs between C2H579Br spike and other
brominated hydrocarbons:
Species-specific IDMS is possible !
Bond strength: C - I < C - Br < C - Cl < C - F
0
1000
2000
3000
4000
5000
6000
7000
CHBr 3
C 4 H 9 Br
CH 2 BrCl
C 2 H 5 Br
81 B
r Int
ensi
ty (c
ps)
81Br chromatogram
0 5 10 15 20 25 30 35 0
1000
2000
3000
4000
5000
6000
7000
CHBr 3
C 4 H 9 Br CH 2 BrCl
79 B
r Int
ensi
ty (c
ps)
Retention time (min)
79Br chromatogram C2H5Br
Existing experience with the application of species-specific determination of elemental species by ICP-IDMS
Element Isotope Alkylated compounds Inorganic compounds Reference
Br 79Br C2H5Br Br-, BrO3- Heumann
Cr 53Cr CrO42- Kingston,
Heumann
Hg 201Hg CH3Hg+ Donard, Frech, Heumann
I 129I CH3I, C3H7I I-, IO3- Heumann
Pb 206Pb (CH3)3Pb+ Ebdon, Heumann
Se 82Se (CH3)2Se, (CH3)2Se2, SeO32-, SeO4
2- Heumann (CH3)3Se+
Se-methionine Garcia Alonso and Sanz-Medel
Sn 117Sn (C4H9)3Sn+, (C4H9)2Sn2+ Garcia Alonso and Sanz-Medel
Tl 203Tl (CH3)2Tl+ Heumann
Is species-unspecific determination of elemental species necessary by
GC/ICP-IDMS even if volatile compounds are usually
well defined ?
If different species of the same element are to be determined
species-unspecific spiking will avoid synthesis of all spike compounds
Schematic figure of the species-specific and species-unspecific isotope dilution technique for sulfur speciation
(J. Heilmann and K.G. Heumann)
Sample + isotope-labeled analyte for
species-specific spiking technique
GC-Injector
ICP-MS GC capillary
Continuous addition of a species-unspecific spike by
gas cylinder or permeation tube
Units used in the species- unspecific spiking technique
Unspiked sample for species-unspecific
spiking technique
Isotope chromatogram of species-unspecific GC/ICP-IDMS for sulfur species determination in a standard solution using 34S-enriched
dimethyldisulfide
(J. Heilmann and K.G. Heumann)
0
2
4
6
8
10
12
14
16
18
20
9 14 19 24 29
Retention time [min]
34S/
32S
S SCH3
S
S CH3
S
CH3
For quantitative analysis spike flow must be calibrated
Determination of MeHg+ and inorganic Hg2+ in biological materials by species-unspecific ETV/ICP-IDMS
(I. Gelaude, F. Vanhaecke and R. Dams)
Fractionated evaporation of MeHg+ and inorg. Hg by a two-step ETV temperature program
Ar ICP-MS
permeation tube
200Hg (spike)
Isotope dilution of all Hg species by isotope-enriched 200Hg
Water bath
Permeation tube guarantees continuous spike flow into the time-delayed analytes evaporated by ETV
Determination of MeHg+ and inorganic Hg2+ in the certified reference material TORT-2 (lobster) by
species-unspecific ETV/ICP-IDMS
(I. Gelaude, F. Vanhaecke and R. Dams)
Method Concentration (µg Hg/g)
MeHg+ Inorg. Hg Total Hg
ETV/ICP-IDMS
Certified
0.16 ± 0.02 0.12 ± 0.06 0.28 ± 0.05
0.15 ± 0.01 0.27 ± 0.06 -
Summary
Isotope-labeled species must normally be synthesized for species-specific IDMS
Online coupling of ICP-MS with GC and HPLC is technically easy but more difficult for CE
Hyphenated techniques in combination with IDMS are the only possibility to obtain real-time concentrations of species
Because of a lack of alternatives GC/ICP-IDMS and HPLC/ICP-IDMS are the most powerful methods for quantitative elemental speciation and therefore also suitable for routine analysis
Elemental speciation can be carried out by species-specific and species-unspecific ICP-IDMS applying coupling with HPLC, GC and CE
Species-specific IDMS is an ideal tool for method validation
However, spectrometric interferences in ICP-MS can always affect the results