Abstract
We studied the properties of CaCO 3 and phosphate sorption of 36 calcareous soil samples collected across the Mediterranean part of Spain. Owing to its low surface area and to its relatively low phosphate sorption capacity, CaCO 3 did not influence sorption markedly. Other soil components of calcareous soils, such as Fe oxides or silicate clays appear to be quantitatively more important, at least for sorption at low phosphate equilibrium concentrations.
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