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单裂隙砂岩中纳米银颗粒的输运

Transport of silver nanoparticles in single fractured sandstone.

机构信息

Federal Institute for Geoscience and Natural Resources, Stilleweg 2, 30655 Hanover, Germany.

出版信息

J Contam Hydrol. 2018 Feb;209:61-67. doi: 10.1016/j.jconhyd.2018.01.007. Epub 2018 Feb 1.

Abstract

Silver nanoparticles (Ag-NP) are used in various consumer products and are one of the most prevalent metallic nanoparticle in commodities and are released into the environment. Transport behavior of Ag-NP in groundwater is one important aspect for the assessment of environmental impact and protection of drinking water resources in particular. Ag-NP transport processes in saturated single-fractured sandstones using triaxial flow cell experiments with different kind of sandstones is investigated. Ag-NP concentration and size are analyzed using flow field-flow fractionation and coupled SEM-EDX analysis. Results indicate that Ag-NP are more mobile and show generally lower attachment on rock surface compared to experiments in undisturbed sandstone matrix and partially fractured sandstones. Ag-NP transport is controlled by the characteristics of matrix porosity, time depending blocking of attachment sites and solute chemistry. Where Ag-NP attachment occur, it is heterogeneously distributed on the fracture surface.

摘要

银纳米颗粒(Ag-NP)被广泛应用于各种消费品中,是商品中最常见的金属纳米颗粒之一,并被释放到环境中。Ag-NP 在地下水中的迁移行为是评估环境影响和保护饮用水资源的一个重要方面。本研究采用三轴流动池实验,研究了不同类型砂岩中 Ag-NP 在饱和单裂隙砂岩中的迁移过程。利用流场-流分和 SEM-EDX 分析联用技术对 Ag-NP 的浓度和粒径进行了分析。结果表明,与原状砂岩和部分裂隙砂岩相比,Ag-NP 具有更高的迁移性,且通常在岩石表面的附着量较低。Ag-NP 的迁移受基质孔隙率、随时间变化的附着位点堵塞以及溶质化学性质的控制。Ag-NP 的附着是不均匀分布在裂隙表面上的。

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