Computer Science
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Burial diagenesis of siliciclastic reservoirs and control on formation water chemistry
Hydration of forsterite at 1 atm PCO2 and 80 to 120°C - Comparisons of numerical simulations and laboratory experiments to understand the factors that govern the overall mineral transformation rate
Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. II. Rate constants, effective surface area, and the hydrolysis of feldspar
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