Geochemistry
The acid dissociation constant, denoted as $$k_a$$, is a quantitative measure of the strength of an acid in solution. It represents the equilibrium constant for the dissociation of an acid into its conjugate base and hydrogen ions. A higher $$k_a$$ value indicates a stronger acid that dissociates more completely in water, which is important for understanding acid-base reactions and their dynamics in various chemical processes.
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