How do the fundamental chemical principles of thermodynamics and kinetics govern the formation and alteration of sedimentary rocks? Robert A. Berner, a distinguished geochemist, utilizes his expertise in low-temperature geochemistry to construct a rigorous framework for understanding the chemical processes occurring at the Earth's surface. The text integrates physical chemistry with geological observations to explain the precipitation, dissolution, and diagenesis of minerals within sedimentary environments.

Experts recognize this work as a foundational text for graduate-level students and researchers in geochemistry. Readers frequently note the technical density of the prose, which requires a strong background in chemistry to fully comprehend the mathematical models presented.