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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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| Main Authors: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2005
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| Assuntos: | |
| Acesso em linha: | 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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