Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water
<p>Headspace analysis of CO<span class="inline-formula"><sub>2</sub></span> frequently has been used to quantify the concentration of CO<span class="inline-formula"><sub>2</sub></span> in fresh water. According to basic chemic...
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doaj-229a12bd6df54631beab6ecb7c252ebe2021-03-09T10:34:22ZengCopernicus PublicationsBiogeosciences1726-41701726-41892021-03-01181619162710.5194/bg-18-1619-2021Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh waterM. Koschorreck0Y. T. Prairie1J. Kim2R. Marcé3R. Marcé4Department Lake Research, Helmholtz Centre for Environmental Research – UFZ, Brückstrasse 3a, 39114 Magdeburg, GermanyDépartement des Sciences Biologiques, Université du Québec à Montréal, Montréal, Quebec, CanadaDépartement des Sciences Biologiques, Université du Québec à Montréal, Montréal, Quebec, CanadaCatalan Institute for Water Research (ICRA), Emili Grahit 101, 17003 Girona, SpainUniversity of Girona, Girona, Spain<p>Headspace analysis of CO<span class="inline-formula"><sub>2</sub></span> frequently has been used to quantify the concentration of CO<span class="inline-formula"><sub>2</sub></span> in fresh water. According to basic chemical theory, not considering chemical equilibration of the carbonate system in the sample vials will result in a systematic error. By analysing the potential error for different types of water and experimental conditions, we show that the error incurred by headspace analysis of CO<span class="inline-formula"><sub>2</sub></span> is less than 5 % for typical samples from boreal systems which have low alkalinity (<span class="inline-formula"><</span> 900 <span class="inline-formula">µ</span>mol L<span class="inline-formula"><sup>−1</sup></span>), with pH <span class="inline-formula"><</span> 7.5, and high <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span> (<span class="inline-formula">></span> 1000 <span class="inline-formula">µ</span>atm). However, the simple headspace calculation can lead to high error (up to <span class="inline-formula">−</span>300 %) or even impossibly negative values in highly undersaturated samples equilibrated with ambient air, unless the shift in carbonate equilibrium is explicitly considered. The precision of the method can be improved by lowering the headspace ratio and/or the equilibration temperature. We provide a convenient and direct method implemented in an R script or a JMP add-in to correct CO<span class="inline-formula"><sub>2</sub></span> headspace results using separately measured alkalinity.</p>https://bg.copernicus.org/articles/18/1619/2021/bg-18-1619-2021.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
M. Koschorreck Y. T. Prairie J. Kim R. Marcé R. Marcé |
spellingShingle |
M. Koschorreck Y. T. Prairie J. Kim R. Marcé R. Marcé Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water Biogeosciences |
author_facet |
M. Koschorreck Y. T. Prairie J. Kim R. Marcé R. Marcé |
author_sort |
M. Koschorreck |
title |
Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water |
title_short |
Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water |
title_full |
Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water |
title_fullStr |
Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water |
title_full_unstemmed |
Technical note: CO<sub>2</sub> is not like CH<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>CO<sub>2</sub> in fresh water |
title_sort |
technical note: co<sub>2</sub> is not like ch<sub>4</sub> – limits of and corrections to the headspace method to analyse <i>p</i>co<sub>2</sub> in fresh water |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2021-03-01 |
description |
<p>Headspace analysis of CO<span class="inline-formula"><sub>2</sub></span> frequently has been used
to quantify the concentration of CO<span class="inline-formula"><sub>2</sub></span> in fresh water. According to basic
chemical theory, not considering chemical equilibration of the carbonate
system in the sample vials will result in a systematic error. By analysing
the potential error for different types of water and experimental conditions, we show that the error incurred by headspace analysis of CO<span class="inline-formula"><sub>2</sub></span> is less
than 5 % for typical samples from boreal systems which have low alkalinity
(<span class="inline-formula"><</span> 900 <span class="inline-formula">µ</span>mol L<span class="inline-formula"><sup>−1</sup></span>), with pH <span class="inline-formula"><</span> 7.5, and high
<span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span> (<span class="inline-formula">></span> 1000 <span class="inline-formula">µ</span>atm). However, the simple headspace
calculation can lead to high error (up to <span class="inline-formula">−</span>300 %) or even impossibly
negative values in highly undersaturated samples equilibrated with ambient
air, unless the shift in carbonate equilibrium is explicitly considered. The
precision of the method can be improved by lowering the headspace ratio
and/or the equilibration temperature. We provide a convenient and direct
method implemented in an R script or a JMP add-in to correct CO<span class="inline-formula"><sub>2</sub></span>
headspace results using separately measured alkalinity.</p> |
url |
https://bg.copernicus.org/articles/18/1619/2021/bg-18-1619-2021.pdf |
work_keys_str_mv |
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