Geochemistry
Mineral solubility refers to the ability of a mineral to dissolve in a solvent, typically water, which is influenced by temperature, pressure, and the presence of other dissolved substances. The extent of solubility can affect various geochemical processes such as weathering, nutrient cycling, and the formation of secondary minerals. Understanding mineral solubility is crucial for interpreting geochemical interactions in natural systems and has implications for environmental science, agriculture, and resource management.
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