High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors
To investigate CO 2 chemistry in ocean water with greater time‐space resolutions, we developed measurement systems, which have state‐of‐the‐art precision but an order of magnitude or better increase in the frequency of analysis, for carbon dioxide partial pressures (P CO2 ) and total carbon dioxide...
Published in: | Limnology and Oceanography: Methods |
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crwiley:10.4319/lom.2004.2.356 2024-09-30T14:24:39+00:00 High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors Hales, Burke Chipman, David Takahashi, Taro 2004 http://dx.doi.org/10.4319/lom.2004.2.356 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flom.2004.2.356 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lom.2004.2.356 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography: Methods volume 2, issue 11, page 356-364 ISSN 1541-5856 1541-5856 journal-article 2004 crwiley https://doi.org/10.4319/lom.2004.2.356 2024-09-03T04:26:11Z To investigate CO 2 chemistry in ocean water with greater time‐space resolutions, we developed measurement systems, which have state‐of‐the‐art precision but an order of magnitude or better increase in the frequency of analysis, for carbon dioxide partial pressures (P CO2 ) and total carbon dioxide concentrations (T CO2 ) in seawater. The P CO2 system was based on equilibration of a CO 2 ‐free carrier gas stream with aqueous carbon dioxide in a flowing seawater sample stream using a commercially available membrane contactor unit normally employed in industrial applications followed by nondispersive infrared (NDIR) absorbance detection of the CO 2 in the exit carrier gas. The T CO2 system was based on injection of a small‐volume seawater sample loop (~1 mL) into an acid (0.1 N HCl) liquid carrier stream to convert all carbonate and bicarbonate ions to aqueous carbon dioxide; this acidified sample was then passed through a custom‐made small‐volume membrane contactor unit where the sample's P CO2 was determined by equilibration of a CO 2 ‐free carrier gas followed by NDIR detection. Results from lab tests and a field experiment in the Ross Sea polynya, Antarctica, are presented. The P CO2 system was determined to have a response time of about 3 s and precision of better than 1 µatm. The T CO2 system had a maximum analysis rate of one sample per 36 s, and reproducibility was determined to be better than 0.2% for a period of hours. Article in Journal/Newspaper Antarc* Antarctica Ross Sea Wiley Online Library Ross Sea Limnology and Oceanography: Methods 2 11 356 364 |
institution |
Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
To investigate CO 2 chemistry in ocean water with greater time‐space resolutions, we developed measurement systems, which have state‐of‐the‐art precision but an order of magnitude or better increase in the frequency of analysis, for carbon dioxide partial pressures (P CO2 ) and total carbon dioxide concentrations (T CO2 ) in seawater. The P CO2 system was based on equilibration of a CO 2 ‐free carrier gas stream with aqueous carbon dioxide in a flowing seawater sample stream using a commercially available membrane contactor unit normally employed in industrial applications followed by nondispersive infrared (NDIR) absorbance detection of the CO 2 in the exit carrier gas. The T CO2 system was based on injection of a small‐volume seawater sample loop (~1 mL) into an acid (0.1 N HCl) liquid carrier stream to convert all carbonate and bicarbonate ions to aqueous carbon dioxide; this acidified sample was then passed through a custom‐made small‐volume membrane contactor unit where the sample's P CO2 was determined by equilibration of a CO 2 ‐free carrier gas followed by NDIR detection. Results from lab tests and a field experiment in the Ross Sea polynya, Antarctica, are presented. The P CO2 system was determined to have a response time of about 3 s and precision of better than 1 µatm. The T CO2 system had a maximum analysis rate of one sample per 36 s, and reproducibility was determined to be better than 0.2% for a period of hours. |
format |
Article in Journal/Newspaper |
author |
Hales, Burke Chipman, David Takahashi, Taro |
spellingShingle |
Hales, Burke Chipman, David Takahashi, Taro High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
author_facet |
Hales, Burke Chipman, David Takahashi, Taro |
author_sort |
Hales, Burke |
title |
High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
title_short |
High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
title_full |
High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
title_fullStr |
High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
title_full_unstemmed |
High‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
title_sort |
high‐frequency measurement of partial pressure and total concentration of carbon dioxide in seawater using microporous hydrophobic membrane contactors |
publisher |
Wiley |
publishDate |
2004 |
url |
http://dx.doi.org/10.4319/lom.2004.2.356 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flom.2004.2.356 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lom.2004.2.356 |
geographic |
Ross Sea |
geographic_facet |
Ross Sea |
genre |
Antarc* Antarctica Ross Sea |
genre_facet |
Antarc* Antarctica Ross Sea |
op_source |
Limnology and Oceanography: Methods volume 2, issue 11, page 356-364 ISSN 1541-5856 1541-5856 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lom.2004.2.356 |
container_title |
Limnology and Oceanography: Methods |
container_volume |
2 |
container_issue |
11 |
container_start_page |
356 |
op_container_end_page |
364 |
_version_ |
1811641809810489344 |