A carregar...

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...

ver descrição completa

Na minha lista:
Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Sulpis, Olivier, Boudreau, Bernard P., Mucci, Alfonso, Jenkins, Chris, Trossman, David S., Arbic, Brian K., Key, Robert M.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2018
Assuntos:
Acesso em linha: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
Tags: Adicionar Tag
Sem tags, seja o primeiro a adicionar uma tag!