Geochemistry
Titration is a quantitative analytical method used to determine the concentration of an unknown solution by reacting it with a solution of known concentration. This technique involves the gradual addition of the titrant to the analyte until a reaction endpoint is reached, often indicated by a color change or pH shift. Titration is significant in water chemistry and acid-base reactions, as it allows for precise measurement of chemical concentrations, aiding in the analysis of environmental samples and the understanding of acid-base equilibria.
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