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: Intensive plastic mulch application has improved agricultural productivity. However, fragmentary microplastic residues accumulate in soils, potentially degrading surface soil hydraulic properties while being prone to overland transport. As soil surfaces act as dynamic pollutant sources for both overland and subsurface transport during erosive rainfall, both transport processes are mechanistically coupled and must be conjunctively understood to characterize microplastic fate. Accordingly, a flume experiment was conducted to simulate coupled overland and subsurface microplastic transport at two slopes (5°, 10°) under 1.5 mm min -1 rainfall intensity for 1 h. The uppermost 1 cm of soil was spiked with 0.025% by weight microplastics, comprising a mixture of debris and particles, to simulate agricultural plastic mulch residues. Results showed that 4.8% and 6.4% of microplastics were transported overland at 5° and 10° slope, respectively. The overland transported microplastics occurred mostly within runoff, while a small proportion settled with the eroded soil sediments. The transport behavior of debris and particles differed substantially, including the sensitivities of the overland and subsurface fluxes to slope, temporal dynamics of concentration profiles within the runoff and eroded sediment, and mass distributions across runoff, sediment, and various soil depths. Therefore, microplastics are susceptible to overland transport due to low subsurface mobility, which may be most severe in arid croplands, where soil erosion, plastic mulching, and limited rainwater infiltration are prevalent. This study advances understanding of how rainfall-induced soil erosion may drive expanding shallow soil microplastic pollution, which is susceptible to further erosive rainfall, and distinct for microplastics of different characteristics.
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Tang et al. (2026) studied this question.
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