4.7 Article

The spatial distribution and abundance of microplastics in lake waters and ice during ice-free and ice-covered periods

Journal

ENVIRONMENTAL POLLUTION
Volume 323, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2023.121268

Keywords

Microplastics; Spatial -temporal variations; Cold lacustrine ecosystems; Lake ulansuhai

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Understanding the impact of lake ice on microplastics (MPs) in lake waters is crucial for addressing plastic pollution. This study found that ice formation reduced the abundance of MPs in lake waters, while increasing their concentration in the ice. Additionally, MPs showed a distinct spatial pattern during the ice-covered period compared to the ice-free period.
Understanding the spatial distribution and characteristics of microplastics (MPs) in lake waters is essential to assessing and addressing lacustrine MP pollution. This study investigated how lake ice affects the abundance, spatial distribution, and characteristics (size, shape) of MPs in Lake Ulansuhai by analyzing samples collected at ten sites uniformly distributed throughout the lake during ice-free and ice-covered periods. The abundance of MPs ranged between 204 +/- 28 and 1224 +/- 185 n center dot L-1 in lake waters during the ice-free period, and from 34 +/- 8 to 216 +/- 21 n center dot L-1 and 269 +/- 84 to 915 +/- 117 n center dot L-1 in water and ice during the ice-covered period, respectively. During the ice-covered period, MPs were 2.74-8.14 times higher in the ice than in water beneath the ice. Ice formation decreased MP abundance in lake waters, in part, by incorporating a relatively high percentage of MPs into the ice mass during freezing and by inhibiting atmospheric MPs from reaching the lake waters. The abundance of MPs in the water during the ice-free period was 4.50-11.30 times greater than during the ice -covered period. Seasonal variations in MP shape also occurred; the proportion of fibrous MPs in water decreased during the ice-covered period. Variations in MP abundance were partly due to differences in sedi-mentation rates; the settling of fibrous MPs is slower, making it easier for them to be captured during the for-mation of surface ice. Spatially, MPs were uniformly distributed during the ice-free period, but exhibited a spatially distinct pattern during ice-covered periods, when MPs in lake waters were higher in the northeast and lower in the southwest portions of the lake. During the ice-free period, small MPs (0.05-0.5 mm) were more likely to move with currents in the lake, whereas water velocities were reduced by ice formation, allowing small MPs to accumulate near the lake inlet.

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