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...

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Published in:Limnology and Oceanography: Methods
Main Authors: Hales, Burke, Chipman, David, Takahashi, Taro
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2004
Subjects:
Online Access:http://dx.doi.org/10.4319/lom.2004.2.356
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spelling 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
collection Wiley Online Library
op_collection_id 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
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