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Kinetics of polystyrene nanoplastic deposition on SiO2 and Al2O3 surfaces: Ionic strength effects
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This study examined how salt concentration in water affects the behavior of polystyrene nanoplastics sticking to mineral surfaces (silica and alumina) found in soil. Higher ionic strength caused more particle deposition, suggesting nanoplastics may accumulate more in soils with higher mineral salt content.
Nanoplastic pollution is an emerging environmental threat to the critical zone. The transport of nanoplastic particles in subsurface environments can be determined mainly by soil minerals because they provide surfaces that interact with nanoplastic particles. However, the interactions between mineral surfaces and nanoplastics are poorly understood. In this study, the deposition kinetics of polystyrene-nanoplastic particles onto representative oxide surfaces SiO 2 and Al 2 O 3 at circumneutral pH were investigated using a quartz crystal microbalance, with variations in the ionic strength (0.1–100 mM) of the well-dispersed nanoplastic particles suspension. While polystyrene-nanoplastic particles deposited minimally on the SiO 2 surface at an ionic strength of < 100 mM (∼10 ng/cm 2 ), substantial deposition occurred at 100 mM (3.7 ± 0.4 μg/cm 2 ). On the Al 2 O 3 surface, a significant amount of polystyrene-nanoplastic particle was deposited from the lowest ionic strength (4.5 ± 0.8 μg/cm 2) . The deposition mass at 100 mM NaCl was two times higher (7.2 ± 0.2 μg/cm 2 ) than on the SiO 2 surface, while the deposition rates were similar between the two surfaces (10–15 Hz/min). Our results indicate that alumina most likely exerts a stronger influence than quartz on the transport of nanoplastic particles in soils and groundwater aquifers. The deposition kinetics strongly depends on the mineral surface and solution ionic strength, and these quantitative results can serve as validation data in developing transport modeling of nanoplastic in subsurface environments.
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Researchers used column experiments across three soil types to show that polystyrene nanoplastic transport is governed by soil iron and aluminum oxide content and pH — with high-pH, low-oxide soils allowing up to 97% nanoplastic passage — and that calcium ions and higher ionic strength significantly increase retention, revealing that soil chemistry strongly controls nanoplastic mobility toward groundwater.
Mineral surface-specific nanoplastic adsorption: Insights from quartz crystal microbalance experiment and molecular modeling simulations
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This study investigated how nanoplastics stick to mineral surfaces commonly found in soil and water — specifically quartz (SiO2) and alumina (Al2O3) — using both lab experiments and molecular computer simulations. The two minerals behaved oppositely: higher salt concentrations increased nanoplastic deposition on quartz but reduced it on alumina, explained by differences in hydrophobic versus hydrophilic surface interactions. Understanding these mineral-specific adsorption behaviors is important for predicting how nanoplastics move through soils and aquifers and whether they could reach drinking water sources.
Aggregation and Deposition Kinetics of Polystyrene Microplastics and Nanoplastics in Aquatic Environment
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Researchers measured aggregation and deposition kinetics of 50 nm and 500 nm polystyrene particles under varying ionic strength and pH conditions, finding that both particle sizes aggregated rapidly at elevated salt concentrations and that the smaller nanoplastics were more mobile in column experiments.
Charge mediated interaction of polystyrene nanoplastic (PSNP) with minerals in aqueous phase
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Researchers investigated how polystyrene nanoplastics interact with common soil and sediment minerals, finding that positively charged iron oxide minerals (goethite and magnetite) strongly adsorb nanoplastics via electrostatic attraction and hydrogen bonding, while negatively charged clay minerals do not — providing mechanistic insight into how nanoplastics may accumulate in iron-rich soils and sediments.
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