Determination of carbonate parameters in seawater

The world's oceans are an important sink for increasing anthropogenic CO2 emissions. Since the middle of the 18th century, the world's oceans have absorbed about 41% of anthropogenic CO2. As CO2 forms carbonic acid in water, CO2 absorption also has an effect on seawater pH. This decrease i...

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Main Authors: Frank, C., Fietzek, Peer, Sobin, J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2014
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/24646/
http://www.intoceansys.co.uk/articles-detail.php?iss=0000000041&acl=0000000349
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spelling ftoceanrep:oai:oceanrep.geomar.de:24646 2023-05-15T15:52:31+02:00 Determination of carbonate parameters in seawater Frank, C. Fietzek, Peer Sobin, J. 2014 https://oceanrep.geomar.de/id/eprint/24646/ http://www.intoceansys.co.uk/articles-detail.php?iss=0000000041&acl=0000000349 unknown Frank, C., Fietzek, P. and Sobin, J. (2014) Determination of carbonate parameters in seawater. Open Access International Ocean Systems, 18 (2). info:eu-repo/semantics/openAccess Article NonPeerReviewed 2014 ftoceanrep 2023-04-07T15:13:27Z The world's oceans are an important sink for increasing anthropogenic CO2 emissions. Since the middle of the 18th century, the world's oceans have absorbed about 41% of anthropogenic CO2. As CO2 forms carbonic acid in water, CO2 absorption also has an effect on seawater pH. This decrease in seawater pH - of about 0.1pH units so far - is also known as ocean acidification and it amounts to an increase in acid concentration of approximately 30%. In order to track corresponding changes in the carbonate system there is a need for innovative sensors. Article in Journal/Newspaper Carbonic acid Ocean acidification OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language unknown
description The world's oceans are an important sink for increasing anthropogenic CO2 emissions. Since the middle of the 18th century, the world's oceans have absorbed about 41% of anthropogenic CO2. As CO2 forms carbonic acid in water, CO2 absorption also has an effect on seawater pH. This decrease in seawater pH - of about 0.1pH units so far - is also known as ocean acidification and it amounts to an increase in acid concentration of approximately 30%. In order to track corresponding changes in the carbonate system there is a need for innovative sensors.
format Article in Journal/Newspaper
author Frank, C.
Fietzek, Peer
Sobin, J.
spellingShingle Frank, C.
Fietzek, Peer
Sobin, J.
Determination of carbonate parameters in seawater
author_facet Frank, C.
Fietzek, Peer
Sobin, J.
author_sort Frank, C.
title Determination of carbonate parameters in seawater
title_short Determination of carbonate parameters in seawater
title_full Determination of carbonate parameters in seawater
title_fullStr Determination of carbonate parameters in seawater
title_full_unstemmed Determination of carbonate parameters in seawater
title_sort determination of carbonate parameters in seawater
publishDate 2014
url https://oceanrep.geomar.de/id/eprint/24646/
http://www.intoceansys.co.uk/articles-detail.php?iss=0000000041&acl=0000000349
genre Carbonic acid
Ocean acidification
genre_facet Carbonic acid
Ocean acidification
op_relation Frank, C., Fietzek, P. and Sobin, J. (2014) Determination of carbonate parameters in seawater. Open Access International Ocean Systems, 18 (2).
op_rights info:eu-repo/semantics/openAccess
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