Babak Dialameh, Kevin W. King, Jedediah H. Stinner, Manal H. Askar, Chad J. Penn, Mark R. Williams, Margaret M. Kalcic, Vinayak S. Shedekar
Agricultural phosphorus (P) hotspots can be defined as localized areas of elevated soil test P (STP) concentration resulting from P application rates exceeding crop removal. They typically form over prolonged periods or following intensive P application and may enhance edge-of-field P loss. This study evaluated the individual and combined impacts of P hotspots and controlled drainage (CD) on edge-of-field P losses through subsurface drainage using a paired-field before–after–control–impact (BACI) design. Two adjacent farm fields in the Western Lake Erie Basin (Ohio) with identical agronomic management practices were monitored over four years (2020–2023). A P hotspot was induced in the “impact field” by applying P at 102 kg P/ha per event over two application events to 8% of the drainage area. Consequently, the surface layer (0–5 cm) STP concentration within the hotspot doubled (55 to 119 mg P/kg). Moreover, the average weekly total P (TP) concentration in subsurface drainage increased from 0.33 to 0.42 mg/L but increases in dissolved reactive P (DRP) were not statistically significant. When CD management was applied to the hotspot field, average weekly drainage discharge decreased by 79% (0.27 to 0.05 mm). During this period, average weekly DRP and TP concentrations in drainage discharge significantly increased, yet the reduced drainage volume led to an 89% decrease in weekly DRP and a 97% decrease in TP loads. These results indicate that reduced drainage discharge under CD resulted in substantially lower subsurface P loads, despite elevated P concentrations.