The intensity of the reactions of the phosphate fertilizer in the soil should vary in function of the different management systems. The study had the objective of evaluating the modifications in the inorganic fractions of P as affected by soil tillage and crop sequence. In May 1997, three soil layers of four long-term field experiments, involving no-tillage and conventional tillage with different crop sequences, were sampled. The total P and six fractions of inorganic P were evaluated. The medium content of total P was much higher than the native P. Total P increased in the upper soil layer under no-tillage. Available (resin and NaHCO3 0.5 mol L-1) and nonlabile inorganic P (HCl 1.0 mol L-1) were higher in the surface layer under no-tillage than in conventional tillage. The highest concentrations of inorganic P were moderately labile (NaOH 0.1 mol L-1). The crop sequences did not influence the fractions of inorganic P.
tillage; phosphate fertilizers; crops; nutrient uptake
