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氧化石墨烯促进 Pb 和 Cd 在饱和多孔介质中的迁移。

Graphene oxide-facilitated transport of Pb and Cd in saturated porous media.

机构信息

College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China.

College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China; Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling 712100, China.

出版信息

Sci Total Environ. 2018 Aug 1;631-632:369-376. doi: 10.1016/j.scitotenv.2018.03.036. Epub 2018 Mar 16.

Abstract

This paper provides an overview of the effect of graphene oxide (GO) on sorption, transport, and remobilization of Pb and Cd ions in saturated porous media. The affinity of GO to Pb and Cd ions was investigated via kinetic and isothermal sorption experiments. Laboratory packed-column experiments were also conducted to investigate the cotransport of Pb and Cd ions with GO across a quartz sand matrix. In addition, the Pb- and Cd-preequilibrated sand column was sequentially flushed with GO to test its remobilization effect on these ions. GO exhibited a high affinity toward both Pb and Cd ions with maximum sorption capacities of 1428.57 and 911.43mgg, respectively. On the other hand, while GO improved the transport ability of Pb and Cd, both ions reduced the mobility of GO in saturated porous media. Data from the elution experiment revealed that the high affinity of GO toward the metal ions led to the remobilization of the presorbed Pb and Cd ions onto the quartz sand surfaces and their concurrent migration across the sand column. XDLVO (Extended Derjaguin-Landau-Verwey-Overbeek) calculations were employed to interpret the GO transport behavior in the column wells. The cotransport of Pb and Cd ions with GO in the saturated quartz sand was successfully simulated by the advection-dispersion-reaction equation. Findings from this study provide an insight on the potential implications of remobilization and spread of pollutants by nanomaterials existing in vulnerable ecosystems.

摘要

本文概述了氧化石墨烯(GO)对饱和多孔介质中 Pb 和 Cd 离子的吸附、迁移和再移动的影响。通过动力学和等温吸附实验研究了 GO 对 Pb 和 Cd 离子的亲和力。还进行了实验室填充柱实验,以研究 Pb 和 Cd 离子与 GO 在石英砂基质中的共迁移。此外,还对 Pb 和 Cd 预平衡的砂柱进行了顺序冲洗,以测试 GO 对这些离子的再移动效果。GO 对 Pb 和 Cd 离子表现出高亲和力,最大吸附容量分别为 1428.57 和 911.43mgg。另一方面,尽管 GO 提高了 Pb 和 Cd 的迁移能力,但两种离子都降低了 GO 在饱和多孔介质中的迁移能力。洗脱实验的数据表明,GO 对金属离子的高亲和力导致预吸附的 Pb 和 Cd 离子重新移动到石英砂表面,并与它们一起穿过砂柱迁移。XDLVO(扩展的德加古林-兰德维维尔-奥弗贝克)计算被用来解释柱井中 GO 的传输行为。通过对流-弥散-反应方程成功模拟了 Pb 和 Cd 离子与 GO 在饱和石英砂中的共迁移。本研究的结果提供了对存在于脆弱生态系统中的纳米材料的污染物再移动和扩散的潜在影响的深入了解。

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