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PolymerType, Oxidation, Size, and Abundance of Microplasticsin Subsoils versus Topsoils with Varying Land Use in Beijing, China

Figshare 2025
Liuwei Wang (9593775), Caide Huang (21575043), Junhao Cao (12907034), Pingfan Zhou (12633099), Siqi Han (849725), Guangyu Qu (21575046), Michael S. Bank (2315566), Deyi Hou (536277)

Summary

Researchers examined polymer type, size, oxidation state, and abundance of microplastics (20-500 um) in topsoil and subsoils down to 100 cm across six land use types in Beijing using Laser Direct Infrared Chemical Imaging Spectroscopy, identifying 6,085 particles spanning 11 polymer types. Subsoil microplastics were found at lower abundance but were surprisingly larger and less oxidised than topsoil particles, suggesting size-selective vertical transport and reduced weathering at depth.

Study Type Environmental

The occurrence of microplastics (MPs) in topsoil is well documented; however, recent evidence has also shown that MPs can reach the subsoil, which may eventually enter groundwater aquifers posing a potential threat to drinking water. In this study, we examined polymer-type specific, small-sized MPs (20–500 μm) in both topsoil (5 cm) and subsoil (50 and 100 cm) in the megacity of Beijing, China, using Laser Direct Infrared (LDIR) Chemical Imaging Spectroscopy, focusing on variation in abundance, size, polymer type, and oxidation characteristics across 6 land use types. A total of 6085 MP particles with 11 polymer types were identified. MP abundance in subsoils was significantly lower, and they were surprisingly larger in size and less oxidized. MP distribution in subsoils was enhanced in fine-textured and iron (Fe)-depleted soils. Based on these findings, we conducted additional column migration experiments using different textured vadose zones, either with or without hematite, as a typical Fe oxide. Two scenarios were set, including continuous water infiltration and wet–dry cycling conditions. Field data strongly reflected our lab experiments under wet–dry cycling, suggesting that preferential penetration rather than filtration served as the likely primary mechanism of MP occurrence in subsoil.

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