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- W2327537531 abstract "Formation and transformation of clay minerals occur ubiquitously at the interface between mineral and water in the upper part of the Earth crust. The solution-mediated reactions pertaining to clay minerals are characterized by a consecutive transformation from metastable phases toward final stable phases based on the Ostwald's step rule and by the phase transformations via dissolution and recrystallization processes. Two examples have been introduced in this communication: one is the allophane→halloysite→kaolinite reaction series in weathering and the other is the smectite→illite/smectite interstratified minerals→illite reaction series in diagenesis. Understanding of the kinetics of these reactions in natural open systems are only qualitative at present; it is necessary in future to accumulate more data in terms of the rates and mechanisms of dissolution and growth of these minerals in order to understand quantitatively the dynamics of the solution-mediated geochemical reactions." @default.
- W2327537531 created "2016-06-24" @default.
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- W2327537531 date "1996-01-01" @default.
- W2327537531 modified "2023-09-26" @default.
- W2327537531 title "Solution-mediated Phase Transformations of Clay Minerals." @default.
- W2327537531 doi "https://doi.org/10.2465/gkk1952.25.189" @default.
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