Evaluation of P availability from Fe and A1 labelled (32P) phosphates

Synthetically Fe and A1 labelled phosphates (32P) show a certain amount of available P to the plants when applied to Sao Paulo State soils. This availability decreases from considered amorphous A1-phosphate (A1-P sub(am)) to A1 phosphate with a certain cristalinity grade (A1-P sub(cr)) and than from this to Fe-P sub(am) followed by Fe-P sub(cr), and it is influenced by both the soil characteristics and mainly by the iron constituents of the samples. In this way, one can not expect that the 0,05 N2H SO4 and the CHANG and JACKSON (1957a) solutions can define properly the available P of these soils. The addition of lime to the soils do not drive to a better P absorption by the plants and its effects are dubious