Soil Use and Management · 1998 · 47 citations · 29 references
AgricultureAgronomySoil SciencesNutrient CyclingSoil BiogeochemistrySoil FertilityPhosphorus CyclePhosphorus CyclingPhosphorus ManagementPhosphorus NutritionSoil Fertility DynamicsSoil Nutrient CyclingAvailable Soil PhosphorusContinuous CultivationFractionationPhosphate FertilizersPhosphorus FertilizationResidual PhosphorusSoil Phosphorus DynamicsSoil Phosphorus Fractionation
Abstract. We examined the dynamics of inorganic P (P i ) and organic P (P o ) pools of a savanna Alfisol under continuous cultivation complemented with nitrogen (N) and phosphorus (P) fertilizers with or without cow manure (D), using a modified Hedly fractionation. Continuous cultivation without P fertilizer decreased the concentration of P i and P o , pools including the residual P fraction compared with an unfertilized treatment with natural vegetation. Adding P fertilizers alone or in combination with D (P, NPK, D+P, D+NP and D+NPK) increased the concentration of labile P i pools, but decreased the concentration of P o , pools and the residual P fraction. The tendency of the residual P fraction to decrease along with P o pools suggested that the residual P fraction was largely P o . This is consistent with the correlation between the residual P fraction and total P o ( r =0.74 ** ) and the residual P fraction and organic carbon content ( r =0.47 ** ). Analysis of the relationships between plant available P, estimated by resin‐extractable P, and the more stable P i and P o , pools indicated that 85% of the variation in resin‐P was atiributable to the hydroxide extractable P i , (OH‐P i ) and HCI‐P i which acted as sinks for fertilizer‐P. The contribution of the residual P fraction to resin‐P was indirect via bicarbonate‐extractable P o (HCO 3 ‐P o ) and OH‐P o . These results also clarify why attempts to find P extraction methods which correlate well with response to P and to P uptake in the savanna have given inconsistent results.
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