Abstract
Chemical thermodynamics augmented by the Gay-Lussac-Ostwald step rule provides a theoretical approach to weathering phenomena in soils that requires few ad hoc constitutive assumptions. The efficacy of this approach is illustrated with several examples of natural and anthropogenically-induced weathering reactions involving kaolinite. In soils, kaolinite exhibits a continuum of structural disorder that is reflected by a corresponding spectrum of solubility product constants. The composition of the soil solution vis-à-vis this spectrum can be interpreted with the help of the step rule. The concept of a soil kaolinite continuum appears necessary to the evaluation of activity-ratio diagrams and other thermodynamic constructs.
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Sposito, G. (1985). Chemical Models of Weathering in Soils. In: Drever, J.I. (eds) The Chemistry of Weathering. Nato ASI Series, vol 149. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5333-8_1
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DOI: https://doi.org/10.1007/978-94-009-5333-8_1
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