Significant contribution of dissolved organic matter to seawater alkalinity
The present study shows a previously undocumented role of dissolved organic matter in the marine carbonate system. During photosynthesis, phytoplankton release dissolved organic compounds containing basic functional groups that readily react with protons during seawater titration, and thereby contri...
Published in: | Geophysical Research Letters |
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Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/27799 https://doi.org/10.1029/2009GL040271 |
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ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/27799 2023-05-15T15:52:40+02:00 Significant contribution of dissolved organic matter to seawater alkalinity Kim, HC Lee, K 환경공학부 10056383 Lee, K 2009-10-20 https://oasis.postech.ac.kr/handle/2014.oak/27799 https://doi.org/10.1029/2009GL040271 English eng AMER GEOPHYSICAL UNION GEOPHYSICAL RESEARCH LETTERS 36 L20603 SCI급, SCOPUS 등재논문 SCI Geosciences, Multidisciplinary Geology 0094-8276 2009-OAK-0000019357 https://oasis.postech.ac.kr/handle/2014.oak/27799 doi:10.1029/2009GL040271 10355 GEOPHYSICAL RESEARCH LETTERS, v.36, pp.L20603 - L20603 000271129500006 2-s2.0-72149095129 CARBONIC-ACID DISSOCIATION-CONSTANTS TITRATION ALKALINITY PHYTOPLANKTON DIOXIDE GROWTH PH Article ART 2009 ftponangunivst https://doi.org/10.1029/2009GL040271 2022-10-20T20:18:05Z The present study shows a previously undocumented role of dissolved organic matter in the marine carbonate system. During photosynthesis, phytoplankton release dissolved organic compounds containing basic functional groups that readily react with protons during seawater titration, and thereby contribute to alkalinity (a measure of buffering capacity). The magnitude of the contribution of dissolved organic compounds to seawater alkalinity is species dependent, suggesting that individual phytoplankton species exude dissolved organic compounds with unique proton accepting capacities. Our study shows that dissolved organic matter produced by marine phytoplankton during photosynthesis is a newly identified buffering component in the ocean, and indicates that the contribution of dissolved organic matter to seawater alkalinity can be significant in the biologically productive upper ocean, where to date it has been unrecognized or considered insignificant. Citation: Kim, H.-C., and K. Lee (2009), Significant contribution of dissolved organic matter to seawater alkalinity, Geophys. Res. Lett., 36, L20603, doi:10.1029/2009GL040271. X 1 1 45 47 scie scopus Article in Journal/Newspaper Carbonic acid Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Geophysical Research Letters 36 20 |
institution |
Open Polar |
collection |
Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) |
op_collection_id |
ftponangunivst |
language |
English |
topic |
CARBONIC-ACID DISSOCIATION-CONSTANTS TITRATION ALKALINITY PHYTOPLANKTON DIOXIDE GROWTH PH |
spellingShingle |
CARBONIC-ACID DISSOCIATION-CONSTANTS TITRATION ALKALINITY PHYTOPLANKTON DIOXIDE GROWTH PH Kim, HC Lee, K Significant contribution of dissolved organic matter to seawater alkalinity |
topic_facet |
CARBONIC-ACID DISSOCIATION-CONSTANTS TITRATION ALKALINITY PHYTOPLANKTON DIOXIDE GROWTH PH |
description |
The present study shows a previously undocumented role of dissolved organic matter in the marine carbonate system. During photosynthesis, phytoplankton release dissolved organic compounds containing basic functional groups that readily react with protons during seawater titration, and thereby contribute to alkalinity (a measure of buffering capacity). The magnitude of the contribution of dissolved organic compounds to seawater alkalinity is species dependent, suggesting that individual phytoplankton species exude dissolved organic compounds with unique proton accepting capacities. Our study shows that dissolved organic matter produced by marine phytoplankton during photosynthesis is a newly identified buffering component in the ocean, and indicates that the contribution of dissolved organic matter to seawater alkalinity can be significant in the biologically productive upper ocean, where to date it has been unrecognized or considered insignificant. Citation: Kim, H.-C., and K. Lee (2009), Significant contribution of dissolved organic matter to seawater alkalinity, Geophys. Res. Lett., 36, L20603, doi:10.1029/2009GL040271. X 1 1 45 47 scie scopus |
author2 |
환경공학부 10056383 Lee, K |
format |
Article in Journal/Newspaper |
author |
Kim, HC Lee, K |
author_facet |
Kim, HC Lee, K |
author_sort |
Kim, HC |
title |
Significant contribution of dissolved organic matter to seawater alkalinity |
title_short |
Significant contribution of dissolved organic matter to seawater alkalinity |
title_full |
Significant contribution of dissolved organic matter to seawater alkalinity |
title_fullStr |
Significant contribution of dissolved organic matter to seawater alkalinity |
title_full_unstemmed |
Significant contribution of dissolved organic matter to seawater alkalinity |
title_sort |
significant contribution of dissolved organic matter to seawater alkalinity |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2009 |
url |
https://oasis.postech.ac.kr/handle/2014.oak/27799 https://doi.org/10.1029/2009GL040271 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_relation |
GEOPHYSICAL RESEARCH LETTERS 36 L20603 SCI급, SCOPUS 등재논문 SCI Geosciences, Multidisciplinary Geology 0094-8276 2009-OAK-0000019357 https://oasis.postech.ac.kr/handle/2014.oak/27799 doi:10.1029/2009GL040271 10355 GEOPHYSICAL RESEARCH LETTERS, v.36, pp.L20603 - L20603 000271129500006 2-s2.0-72149095129 |
op_doi |
https://doi.org/10.1029/2009GL040271 |
container_title |
Geophysical Research Letters |
container_volume |
36 |
container_issue |
20 |
_version_ |
1766387783431094272 |