Size-dependent transport and retention of micron-sized plastic spheres in natural sand saturated with seawater

海水 自然(考古学) 球体 岩土工程 保水性 环境科学 地质学 土壤科学 海洋学 土壤水分 工程类 航空航天工程 古生物学
作者
Zhiqiang Dong,Yuping Qiu,Wen Zhang,Zhenglong Yang,Wei Li
出处
期刊:Water Research [Elsevier BV]
卷期号:143: 518-526 被引量:172
标识
DOI:10.1016/j.watres.2018.07.007
摘要

A series of one-dimensional column experiments were conducted to investigate the transport and retention of micron-sized plastic spheres (MPs) with diameters of 0.1–2.0 μm in seawater-saturated sand. In seawater with salinity of 35 PSU (practical salinity units), the mass percentages recovered from the effluent (Meff) of the larger MPs increased from 13.6% to 41.3%, as MP size decreased from 2.0 μm to 0.8 μm. This occurred because of the gradual reduction of physical straining effect of MPs in the pores between sands. The smaller MPs (0.6, 0.4, and 0.1 μm) showed the stronger inhibition of MPs mobility, with Meff values of 11.5%, 11.9%, and 9.8%, respectively. This was due to the lower energy barriers (from 108 kBT to 16 kBT) between the smaller MPs and the sand surface, when compared with the larger MPs (from 296 kBT to 161 kBT). In particular, the aggregation of MPs (0.6 or 0.4 μm) triggered a progressive decrease in MP concentration in the effluent. Retention experiments showed that the vertical migration distance of most MP colloids was 0–4 cm at the inlet of column. For 0.6 or 0.4 μm MPs, the particles were concentrated over a 0–2 cm vertical distance. Moreover, the salinity (35–3.5 PSU) did not affect the transport of the larger MPs (2.0–0.8 μm). However, as seawater salinity decreased from 35 PSU to 17.5 or 3.5 PSU, the aggregation of the smaller MPs (0.6–0.1 μm) was dramatically inhibited or completely prevented. Meanwhile, ripening of the sand surface by the MPs (0.6 and 0.4 μm) no longer occurred. By contrast, all MPs in deionized water (0 PSU) achieved complete column breakthroughs because of the strong repulsive energy barrier (from 218 kBT to 4192 kBT) between the MPs and the sand surface. Consequently, we find that the transport and retention of MPs in sandy marine environment strongly relies on both the MP size and the salinity levels.
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