Biogeochemistry
The solubility product, often represented as $$K_{sp}$$, is an equilibrium constant that describes the extent to which a sparingly soluble ionic compound can dissolve in a solution. It is defined as the product of the molar concentrations of the constituent ions, each raised to the power of their coefficients in the balanced dissolution equation. This concept is essential for understanding mineral dissolution kinetics and thermodynamics, as it helps predict the solubility of minerals in various environmental conditions and influences processes such as weathering and nutrient availability.
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