Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay

The potential contribution of redox reactions to acidification in coastal waters is unclear. Here, using measurements from the Chesapeake Bay, the authors show that pH minimum occurs at mid-depths where acids are produced via hydrogen sulfide oxidation in waters mixed upward from anoxic depths.

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Autores principales: Wei-Jun Cai, Wei-Jen Huang, George W. Luther, Denis Pierrot, Ming Li, Jeremy Testa, Ming Xue, Andrew Joesoef, Roger Mann, Jean Brodeur, Yuan-Yuan Xu, Baoshan Chen, Najid Hussain, George G. Waldbusser, Jeffrey Cornwell, W. Michael Kemp
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Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/1e52e3f0370a4c749d437604e8e3da49
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spelling oai:doaj.org-article:1e52e3f0370a4c749d437604e8e3da492021-12-02T17:06:21ZRedox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay10.1038/s41467-017-00417-72041-1723https://doaj.org/article/1e52e3f0370a4c749d437604e8e3da492017-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-00417-7https://doaj.org/toc/2041-1723The potential contribution of redox reactions to acidification in coastal waters is unclear. Here, using measurements from the Chesapeake Bay, the authors show that pH minimum occurs at mid-depths where acids are produced via hydrogen sulfide oxidation in waters mixed upward from anoxic depths.Wei-Jun CaiWei-Jen HuangGeorge W. LutherDenis PierrotMing LiJeremy TestaMing XueAndrew JoesoefRoger MannJean BrodeurYuan-Yuan XuBaoshan ChenNajid HussainGeorge G. WaldbusserJeffrey CornwellW. Michael KempNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-12 (2017)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Wei-Jun Cai
Wei-Jen Huang
George W. Luther
Denis Pierrot
Ming Li
Jeremy Testa
Ming Xue
Andrew Joesoef
Roger Mann
Jean Brodeur
Yuan-Yuan Xu
Baoshan Chen
Najid Hussain
George G. Waldbusser
Jeffrey Cornwell
W. Michael Kemp
Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
description The potential contribution of redox reactions to acidification in coastal waters is unclear. Here, using measurements from the Chesapeake Bay, the authors show that pH minimum occurs at mid-depths where acids are produced via hydrogen sulfide oxidation in waters mixed upward from anoxic depths.
format article
author Wei-Jun Cai
Wei-Jen Huang
George W. Luther
Denis Pierrot
Ming Li
Jeremy Testa
Ming Xue
Andrew Joesoef
Roger Mann
Jean Brodeur
Yuan-Yuan Xu
Baoshan Chen
Najid Hussain
George G. Waldbusser
Jeffrey Cornwell
W. Michael Kemp
author_facet Wei-Jun Cai
Wei-Jen Huang
George W. Luther
Denis Pierrot
Ming Li
Jeremy Testa
Ming Xue
Andrew Joesoef
Roger Mann
Jean Brodeur
Yuan-Yuan Xu
Baoshan Chen
Najid Hussain
George G. Waldbusser
Jeffrey Cornwell
W. Michael Kemp
author_sort Wei-Jun Cai
title Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
title_short Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
title_full Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
title_fullStr Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
title_full_unstemmed Redox reactions and weak buffering capacity lead to acidification in the Chesapeake Bay
title_sort redox reactions and weak buffering capacity lead to acidification in the chesapeake bay
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/1e52e3f0370a4c749d437604e8e3da49
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