Geochemistry
First-order kinetics refers to a reaction rate that is directly proportional to the concentration of a single reactant. In this type of reaction, as the concentration of the reactant decreases, the rate of reaction also decreases, which can be represented mathematically by the equation: $$rac{d[A]}{dt} = -k[A]$$ where $[A]$ is the concentration and $k$ is the rate constant. This relationship indicates that half-lives of reactants remain constant regardless of their initial concentration.
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