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Mechanisms of classical crystal growth theory explain quartz and silicate dissolution behavior

The central control of mineral weathering rates on biogeochemical systems has motivated studies of dissolution for more than 50 years. A complete physical picture that explains widely observed variations in dissolution behavior is lacking, and some data show apparent serious inconsistencies that can...

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Detalles Bibliográficos
Main Authors: Dove, Patricia M., Han, Nizhou, De Yoreo, James J.
Formato: Artigo
Idioma:Inglês
Publicado: National Academy of Sciences 2005
Assuntos:
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC1266142/
https://ncbi.nlm.nih.gov/pubmed/16230632
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0507777102
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