Soil Test Phosphorus and Phosphorus Fractions with Long‐Term Phosphorus Addition and Depletion

Abstract

The fate of fertilizer P in soil during crop production has to be determined to evaluate the long‐term economic value and sustainability of fertilizer practices. We assessed changes in soil test P and soil P fractions with continuous P fertilization and soil P depletion under continuous corn (Zea mays L.) in a Ste. Rosalie clay soil (humic Gleysol; fine, mixed, frigid, Typic Humaquept). Soil samples were analyzed for Mehlich‐3 P (M‐3 P) and P fractions using a modified Hedley's procedure. Soil M‐3 P values remained constant in spite of crop removal in soil not receiving fertilizer for 10 yr. Continuous P fertilization at rates from 44 to 132 P ha−1 yr−1 increased linearly soil M‐3 P, with 6.3 kg P ha−1 of net P addition required to increase M‐3 P by 1 mg P kg−1 Residual fertilizer P in soil resulted from the continuous P addition were found predominately in labile inorganic P (LPi) (NaHCO3–Pi) and moderately labile Pi (MLPi) (NaOH‐Pi). Increased P rates favored soil P transformation from LPi to MLPi, indicating enhanced soil P retention. With P depletion, soil M‐3 P declined in plots previously receiving 132 kg P ha−1 yr−1, with 4.2 kg P ha−1 crop P removal decreasing soil M‐3 P by 1 mg P kg−1 Continuous crop removal of soil residual P (Res‐P) resulted in decreases in soil LPi and increases in MLPi, an indication of increased retention of Res‐P with time. However, moderately stable Pi (HCl‐Pi) remained constant, both with continuous P addition and P depletion. Conversion of residual fertilizer P to less available P forms in soil was a slow process and thus the fate of the Res‐P should be taken into consideration when developing soil nutrient management plans.