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Phosphorus Forms and Desorption Patterns in Heavily Fertilized Calcareous and Limed Acid Soils

Antonio Delgadoa and José Torrentb

a Departamento de Ciencias Agroforestales, Universidad de Sevilla, Ctra. Utrera km 1, 41013 Sevilla, Spain
b Departamento de Ciencias y Recursos Agrícolas y Forestales, Universidad de Córdoba, Apdo. 3048, 14080 Córdoba, Spain



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Fig. 1 Time course of P desorption to mixed cation and anion exchange resins (ACER), plotted as the ratio between the amount of P desorbed (q) and the maximum amount of desorbable P (qmax) against lnt for (a) the limed acid and (b) the calcareous soils. The qmax value was calculated by fitting the Johnson–Mehl equation to the data

 





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