In response to gradually expanding populations and the demand for food, excess anthropogenic phosphorus (P) input to watersheds leads to accumulating large P reservoirs in land systems, which becomes a persistent source of P pollution to aquatic systems, hindering the effectiveness of implementing water quality management. Therefore, clarifying the cycling process of P in watersheds, quantifying the legacy effects of P and identifying the spatial distribution of legacy P are key scientific issues for effectively developing watershed P management. We applied a modification Exploration of Long-tErM Nutrient Trajectories-Phosphorus model in a typical agricultural watershed in eastern China, which can well quantify the dynamics of legacy P over 40 years along the land-aquatic continuum. Modification of P erosion loss module improved the efficiency metrics of the model. The model indicated that the lag time for legacy P effects in the watershed was up to 10 years. P inputs increased by 40% (5.1 kg P ha-1 yr-1-9.8 kg P ha-1 yr-1) between 1980 and 2000 and decreased by 55% (9.8 kg P ha-1 yr-1-3.4 kg P ha-1 yr-1) between 2000 and 2020. Riverine P export fluxes increased from 0.11 kg P ha-1 yr-1to 1.49 kg P ha-1 yr-1 (13-fold increase) from 1980 to 2012, and then decreased to 0.96 kg P ha-1yr-1from 2012-2020 years to 0.96 kg P ha-1 yr-1 (35% decrease). The modification model was effective in clarifying the spatial and temporal distribution of legacy P and proposed an effective method to guide watershed P management.
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Hao et al. (2024) studied this question.
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