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Soil phosphorus and relationship to phosphorus balance under long-term fertilization

机译:在长期施肥下土壤磷和磷平衡的关系

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Temporal changes in the concentrations of plant-available phosphorus (P) in soil (Olsen-P), total soil-P and P activation coefficient (the ratio of Olsen-P to residual-P (i.e. an approximation to total-P)) were measured in plots that received consistent inorganic nitrogen, phosphorus and potassium plus organic fertilizers annually. Maize and winter wheat crops were grown in rotation for 24 years. Olsen-P and P activation coefficient declined significantly in the earlier years (& 12 years) for treatments that did not include any P fertilizer, and increased over the same period for the P-fertilized treatments. The rates of change in the Olsen-P and P activation coefficient values were positively related to P balance. In the later years, the Olsen-P and P activation coefficient plateau values were positively related to the P balance.
机译:土壤(OLSEN-P)中植物可用磷(P)浓度的时间变化,总土壤-P和P激活系数(OLSEN-P与残留-P的比例(即近似为TOTO-P)) 在每年接受一致的无机氮,磷和钾加上有机肥的图中测量。 玉米和冬小麦作物旋转24岁。 奥尔森-P和P激活系数在较早的年龄(& 12年)中显着下降,所述治疗不包括任何P肥料,并且在相同的时间内增加了P-受精处理。 OLSEN-P和P激活系数值的变化率与P平衡呈正相关。 在后期,Olsen-P和P激活系数平台值与P平衡呈正相关。

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