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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: |
National Academy of Sciences
2005
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| 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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