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Current CaCO(3) dissolution at the seafloor caused by anthropogenic CO(2)
Oceanic uptake of anthropogenic CO(2) leads to decreased pH, carbonate ion concentration, and saturation state with respect to CaCO(3) minerals, causing increased dissolution of these minerals at the deep seafloor. This additional dissolution will figure prominently in the neutralization of man-made...
Gorde:
| Argitaratua izan da: | Proc Natl Acad Sci U S A |
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| Egile Nagusiak: | , , , , , , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
National Academy of Sciences
2018
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6243283/ https://ncbi.nlm.nih.gov/pubmed/30373837 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1804250115 |
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