The kinetics of orthophosphate sorption with 25 mineral soils have been experimentally measured under laboratory conditions. The 25 mineral soils represent a wide range of physical and chemical properties. Regression analyses have been performed fitting the experimental data to five kinetic models. The five kinetic models include: a linearized first‐order sorption, a first‐order Freundlich sorption, an empirical function, a diffusion‐limited Langmuir sorption, and a diffusion‐limited Freundlich sorption. Mean correlation coefficients of 0.81, 0.83, 0.84, 0.86, and 0.88 were obtained for the models, respectively.
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Enfield et al. (1976) studied this question.