Determining the longer term decline in plant‐available soil phosphorus from short‐term measured values

Once phosphorus (P) applications stop, it is important to know how long it will take for plant‐available P in soil to decline to a particular level for soils with a history of intensive management. The rate of decline in the absence of applied P can be expressed as a half‐life, that is the time in years for it to halve relative to the lowest level measured in the soil. This knowledge is essential when planning long‐term policies for managing the P status of soils. It is important to farmers who wish to optimize applications of P fertilizers and make better use of accumulated P residues to ensure that plant‐available P does not fall below the critical level for the soil and crop because of the risk of losing yield and the inefficient use of other inputs, especially N fertilizer. Lower levels of plant‐available P are also desirable for environmental and ecological reasons. Allowing plant‐available P to decline to the critical level from unnecessarily high concentrations will reduce the risk from P on eroded soil causing adverse effects of eutrophication in surface water. Low levels of plant‐available P are usually considered necessary for establishing species‐rich grassland. A method for determining the longer term decline in plant‐available soil P from short‐term measured values is presented.