Invariance of apparent equilibrium constants with pH1

The apparent dissociation constants of carbonic acid in seawater are independent of pH for the range 6.5–8.5. These constants, therefore, can be used in the study of geochemical and biochemical processes in the oceans. The arbitrary nature of the pH of seawater does not affect its value in oceanogra...

Full description

Bibliographic Details
Published in:Limnology and Oceanography
Main Authors: Pytkowicz, R. M., Ingle, S. E., Mehrbach, C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1974
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.1974.19.4.0665
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1974.19.4.0665
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1974.19.4.0665
id crwiley:10.4319/lo.1974.19.4.0665
record_format openpolar
spelling crwiley:10.4319/lo.1974.19.4.0665 2024-06-23T07:52:03+00:00 Invariance of apparent equilibrium constants with pH1 Pytkowicz, R. M. Ingle, S. E. Mehrbach, C. 1974 http://dx.doi.org/10.4319/lo.1974.19.4.0665 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1974.19.4.0665 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1974.19.4.0665 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 19, issue 4, page 665-669 ISSN 0024-3590 1939-5590 journal-article 1974 crwiley https://doi.org/10.4319/lo.1974.19.4.0665 2024-06-13T04:20:18Z The apparent dissociation constants of carbonic acid in seawater are independent of pH for the range 6.5–8.5. These constants, therefore, can be used in the study of geochemical and biochemical processes in the oceans. The arbitrary nature of the pH of seawater does not affect its value in oceanographic practice. Article in Journal/Newspaper Carbonic acid Wiley Online Library Limnology and Oceanography 19 4 665 669
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description The apparent dissociation constants of carbonic acid in seawater are independent of pH for the range 6.5–8.5. These constants, therefore, can be used in the study of geochemical and biochemical processes in the oceans. The arbitrary nature of the pH of seawater does not affect its value in oceanographic practice.
format Article in Journal/Newspaper
author Pytkowicz, R. M.
Ingle, S. E.
Mehrbach, C.
spellingShingle Pytkowicz, R. M.
Ingle, S. E.
Mehrbach, C.
Invariance of apparent equilibrium constants with pH1
author_facet Pytkowicz, R. M.
Ingle, S. E.
Mehrbach, C.
author_sort Pytkowicz, R. M.
title Invariance of apparent equilibrium constants with pH1
title_short Invariance of apparent equilibrium constants with pH1
title_full Invariance of apparent equilibrium constants with pH1
title_fullStr Invariance of apparent equilibrium constants with pH1
title_full_unstemmed Invariance of apparent equilibrium constants with pH1
title_sort invariance of apparent equilibrium constants with ph1
publisher Wiley
publishDate 1974
url http://dx.doi.org/10.4319/lo.1974.19.4.0665
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1974.19.4.0665
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1974.19.4.0665
genre Carbonic acid
genre_facet Carbonic acid
op_source Limnology and Oceanography
volume 19, issue 4, page 665-669
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.1974.19.4.0665
container_title Limnology and Oceanography
container_volume 19
container_issue 4
container_start_page 665
op_container_end_page 669
_version_ 1802643240399142912