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Low-Temperature Geochemistry: From Minerals to Surface Waters

Thermodynamics of Aqueous Solutions → Geochemical Modeling of Weathering and Diagenesis

This graduate-level path systematically covers the fundamental principles and processes governing geochemical reactions at Earth's surface. It progresses from thermodynamics and kinetics through mineral dissolution, weathering, clay formation, soil and sediment diagenesis, to the chemistry of surface waters, integrating theoretical foundations with practical applications.