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: | , , |
|---|---|
| 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 |