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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Main Authors: M. Koschorreck, Y. T. Prairie, J. Kim, R. Marcé
Format: Article
Language:English
Published: Copernicus Publications 2021-03-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/18/1619/2021/bg-18-1619-2021.pdf
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spelling 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">&lt;</span> 900 <span class="inline-formula">µ</span>mol L<span class="inline-formula"><sup>−1</sup></span>), with pH <span class="inline-formula">&lt;</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">&gt;</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">&lt;</span> 900 <span class="inline-formula">µ</span>mol L<span class="inline-formula"><sup>−1</sup></span>), with pH <span class="inline-formula">&lt;</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">&gt;</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
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