The Geochemistry of Low-Temperature Systems

The geochemistry of low-temperature systems involves the study of chemical processes and mineral formations occurring in environments like soil, groundwater, and surface waters, typically below 150°C. These processes include how dissolved substances interact, precipitate, or dissolve in water, shaping the mineral content of landscapes and influencing water quality. Factors such as pH, mineral composition, and the presence of gases affect these reactions, helping scientists understand natural resource distribution, environmental changes, and the formation of mineral deposits over time in cooler conditions.