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