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Decreased transport of nano- and micro-plastics in the presence of low-molecular-weight organic acids in saturated quartz sand.

The Science of the total environment 2024
Yanan Liu, Genyao Gu, Jizhe Lu, Luxiang Zhu, Quanyuan Chen, Hyunjung Kim, Jiajun Wang, Peng Ji, Li Cai

Summary

Laboratory experiments showed that common organic acids found in soil — citric, malic, and tartaric acid — significantly reduced the movement of polystyrene nano- and microplastics through saturated sand. This finding suggests that soil organic chemistry influences how microplastics migrate toward groundwater, which has implications for drinking water contamination in agricultural areas.

Polymers

Low-molecular-weight organic acids (LMWOAs) and nano- and micro-plastics (NPs and MPs) are both widely distributed in terrestrial systems. To better understand the influence of LMWOAs on the transport of NPs and MPs, the effects of 0.5 mM citric- (CA), malic- (MA), and tartaric- (TA) acid on the transport of nano- (0.51 μm, PS NPs) and micro- (1.1 μm, PS MPs) polystyrene particles (2 mg L) in saturated quartz sand were investigated. All three LMWOAs decreased the transport of PS NPs and MPs, regardless of ionic composition or strength (0.1-10 mM NaCl and 0.1-1 mM CaCl). Further investigation revealed that the interfacial interactions between PS-quartz sand surfaces and PS-PS were altered by LMWOAs. LMWOAs adsorbed to quartz sand surfaces could serve as new deposition sites, as evidenced by the decreased transport of PS NPs and MPs in quartz sand that was subjected to pre-equilibration with selected MA, the low inhibition of PS transport with low concentrations of LMWOAs (0.1 mM), and also the adsorption of LMWOAs onto quartz sand surfaces by batch experiments. Meanwhile, the adsorption of LMWOAs on PS, hydrodynamic measurement and visual TEM observation together clarified the slight aggregation of PS NPs and MPs in suspensions, inducing the subsequent decrease in transport. Among them, the adsorption of LMWOAs onto quartz sand surfaces was found to be the main factor dominating the decreased transport of both PS NPs and MPs in saturated quartz sand.

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