Abstract:
Flooding the soil resulted in an increase in the content of available P,
Fe-P, AI-P and saloid P, while the concentration of reductant sDluble P, occluded
P and Ca-P showed a gradual decrease. The levels of Fe-P, AI-P, reductant
soluble P, occluded P and available P were high in laterite soil compared to kari
soil. The mean values of saloid P and Ca-P were relatively high in kari soil.