M.P. Andersson, S.M. Ramsheh, A.M. Schade, J.D. Kubicki, M. Turchi, T.R. Walsh, D. Okhrimenko, M. Solvang, S.L.S. Stipp
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引用次数: 0
Abstract
Silicates and aluminosilicates form 95 % of Earth surface rocks and contribute substantially to building materials. Understanding their dissolution is essential for understanding the impact of mineral-H2O-CO2 equilibria and rock weathering on the carbon cycle and for optimising material performance and safety. Predicting dissolution rates is a key but traditional empirical models rely on non-integer reaction orders, which have little meaning, mechanistically and often must be determined for each system separately.
期刊介绍:
Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry.
The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry.
Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry.
The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.