Calcium carbonate corrosivity in an Alaskan inland sea

Ocean acidification is the hydrogen ion increase caused by the oceanic uptake of anthropogenic CO<sub>2</sub>, and is a focal point in marine biogeochemistry, in part, because this chemical reaction reduces calcium carbonate (CaCO<sub>3</sub>) saturation states (Ω) to levels...

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Bibliographic Details
Main Authors: W. Evans, J. T. Mathis, J. N. Cross
Format: Article
Language:English
Published: Copernicus Publications 2014-01-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/11/365/2014/bg-11-365-2014.pdf

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