Relation between soil <scp>P</scp> test values and mobilization of dissolved and particulate <scp>P</scp> from the plough layer of typical <scp>D</scp> anish soils from a long‐term field experiment with applied <scp>P</scp> fertilizers

Abstract

Abstract Accumulation of phosphorus ( P ) in agricultural topsoils can contribute to leaching of P which may cause eutrophication of surface waters. An understanding of P mobilization processes in the plough layer is needed to improve agricultural management strategies. We compare leaching of total dissolved and particulate P through the plough layer of a typical D anish sandy loam soil subjected to three different P fertilizer regimes in a long‐term field experiment established in 1975. The leaching experiment used intact soil columns (20 cm diameter, 20 cm high) during unsaturated conditions. The three soils had small to moderate labile P contents, expressed by water‐extractable P (3.6–10.7 mg/kg), Olsen P (11–28 mg/kg) and degree of P saturation ( DPS ) (25–34%). Mobilization of total dissolved P ( TDP ) increased significantly ( P &lt; 0.05) from the intact soil columns with increasing labile P , whereas the increase in particulate P ( PP ) with increasing labile P content was modest and statistically insignificant. We found concentrations up to 1.5 mg TP/L for the plough layer of this typical D anish sandy loam soil. This highlights that even a moderate labile P content can be a potential source of TDP from the plough layer, and that a lower concentration margin of optimum agronomic P levels should be considered.