How Do Microplastics Affect Physical Properties of Silt Loam Soil under Wetting-Drying Cycles?

Soil physical properties are the main factors that influence soil fertility and directly affect the soil structure and water storage capacity. Microplastics (MPs), which have caused growing concern with respect to soil pollution, have readily been detected in cultivated soils. However, the current data regarding the effects of MPs on soil physical properties during wetting-drying cycles remain insufficient. Therefore, we aimed to explore the effects of different MP particle sizes (25, 150, 550, and 1000 mu m) and concentrations (1, 3, and 5%, w/w) on soil physical properties under indoor wetting-drying cycle conditions. The addition of MPs was found to significantly reduce the saturated hydraulic conductivity and water holding capacity of soil, while impacting the bulk density, water content, and soil particle composition. The properties of soils treated with different MP particle sizes and concentrations exhibited significant differences, while the effects of wetting-drying cycles overshadowed those of MPs. Under the wetting-drying cycles, the saturated hydraulic conductivity and initial soil water content decreased significantly, the soil water holding capacity increased, and the soil bulk density showed a trend of increasing first and then decreasing. We attribute the change to a combination of the microplastics, soil particles, and frequent wetting-drying cycles. In this type of incubation, the constant change in the soil pore proportion results in a change in water and soil porosity, and finally alters the soil physical properties. These findings demonstrate that MP accumulation, together with dynamic environmental conditions, significantly impacts the physical properties of farm land soil.

Automated summary

Soil physical properties, including saturated hydraulic conductivity, water holding capacity, bulk density, and water content, are significantly affected by the addition of microplastics (MPs) under wetting-drying cycle conditions. The effects of different MP particle sizes and concentrations on soil physical properties were observed, but were overshadowed by the effects of wetting-drying cycles. The changes in soil physical properties are attributed to the interaction between MPs, soil particles, and frequent wetting-drying cycles.