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

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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Auteurs principaux: 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
Format: article
Langue:EN
Publié: Nature Portfolio 2017
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Science
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Accès en ligne:https://doaj.org/article/1e52e3f0370a4c749d437604e8e3da49
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https://doaj.org/article/1e52e3f0370a4c749d437604e8e3da49

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