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共存高岭石和针铁矿对水环境污染中氧化石墨烯聚集的影响。

Effect of co-existing kaolinite and goethite on the aggregation of graphene oxide in the aquatic environment.

机构信息

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, 050061, China; Stockbridge School of Agriculture, University of Massachusetts, Amherst, MA, 01003, USA.

Stockbridge School of Agriculture, University of Massachusetts, Amherst, MA, 01003, USA.

出版信息

Water Res. 2016 Oct 1;102:313-320. doi: 10.1016/j.watres.2016.06.050. Epub 2016 Jun 25.

Abstract

Broad applications of graphene oxide (GO) will result in the release of GO into aquatic environments, where clay minerals and metal (hydr)oxides are commonly present. Thereby the interactions between GO and a binary system containing clay minerals and metal (hydr)oxides can occur. We investigated the aggregation of GO with kaolinite and kaolinite-goethite associations (KGAs) in aquatic systems under different pHs, ionic strengths, and GO concentrations. GO suspension was unstable at low pHs, and the aggregation of GO occurred in the presence of KGA-4% and KGA-10% until pH 5 and 6, respectively. Kaolinite decreased the critical coagulation concentration (CCC) of GO at pH 5.5 from around 50 to 20 mM NaCl due to the reduced energy barrier. Heteroaggregation of GO with KGAs was extremely sensitive to ionic strength at pH 5.5, and the CCC of GO in the presence of KGA-10% increased from less than 1 mM NaCl to 5 mM NaCl with the increase of pH from 5.5 to 9. The heteroaggregation extent of GO with KGAs was enhanced firstly, then reduced with the increase of GO concentrations at pH 5.0, which is likely because KGA plates were more efficiently wrapped by large-size GO sheets with increasing GO concentrations. These findings are useful for understanding and predicting the fate of GO in the relatively complicated aquatic and soil environments where binary minerals co-exist.

摘要

氧化石墨烯(GO)的广泛应用将导致其释放到水生环境中,而粘土矿物和金属(氢)氧化物通常存在于其中。因此,GO 与包含粘土矿物和金属(氢)氧化物的二元系统之间可能会发生相互作用。我们研究了在不同 pH 值、离子强度和 GO 浓度下,GO 与高岭石和高岭石-针铁矿组合体(KGA)在水相中的聚集。在低 pH 值下,GO 悬浮液不稳定,在存在 KGA-4%和 KGA-10%的情况下,GO 的聚集分别发生在 pH 值为 5 和 6 时。由于能量障碍降低,高岭石将 GO 在 pH 5.5 时的临界聚沉浓度(CCC)从约 50mM NaCl 降低到 20mM NaCl。在 pH 5.5 时,GO 与 KGA 的异质聚集对离子强度非常敏感,在 pH 从 5.5 增加到 9 时,KGA-10%存在下 GO 的 CCC 从低于 1mM NaCl 增加到 5mM NaCl。在 pH 5.0 时,GO 与 KGA 的异质聚集程度首先增加,然后随着 GO 浓度的增加而降低,这可能是因为随着 GO 浓度的增加,KGA 板更有效地被大尺寸的 GO 片包裹。这些发现有助于理解和预测 GO 在相对复杂的水相和土壤环境中的命运,因为二元矿物共存。

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