Dong Shunan, Sun Yuanyuan, Gao Bin, Shi Xiaoqing, Xu Hongxia, Wu Jianfeng, Wu Jichun
Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China.
Department of Agricultural and Biological Engineering, University of Florida, Gainesville, FL, 32611, USA.
Chemosphere. 2017 Aug;180:506-512. doi: 10.1016/j.chemosphere.2017.04.052. Epub 2017 Apr 18.
In this work, column experiments were conducted to investigate the transport characteristics of graphene oxide (GO) nanoparticles in limestone media under various electrolytes, solution pH, and humic acid (HA) concentration conditions. In the limestone media, GO exhibited relatively low mobility with the mass recovery rate lower than 65.2%, even when solution ionic strength was low. The presence of HA enhanced its mobility. In addition, the presence of S, a divalent anion, also promoted GO transport in limestone media compared to Cl under similar ionic strength conditions through neutralizing more positive charge and thus diminishing the cation bridging. Solution pH showed slight effect on the transport of GO in limestone with the mass recovery range from 40.3% to 51.7%. Over all, decreases in solution pH, HA concentration and increases in solution ionic strength reduced the mobility of GO in the limestone media under the tested conditions. These results indicated both environmental conditions and media characteristics played important roles in controlling GO fate and transport in porous media. The one-site kinetic deposition model was applied to describe the interactions between the GO and limestone media and model simulations fitted the observed experimental data very well. As limestone is an important component of aquiferous media in subsurface, findings from this study elucidated the key factors and processes controlling the fate of GO particles in limestone media, which can inform the prediction and assessment of the risks of GO in groundwater environment.
在本研究中,进行了柱实验,以研究氧化石墨烯(GO)纳米颗粒在不同电解质、溶液pH值和腐殖酸(HA)浓度条件下在石灰岩介质中的传输特性。在石灰岩介质中,即使溶液离子强度较低,GO的迁移率也相对较低,质量回收率低于65.2%。HA的存在提高了其迁移率。此外,在相似离子强度条件下,与Cl相比,二价阴离子S的存在也通过中和更多正电荷从而减少阳离子桥接作用,促进了GO在石灰岩介质中的传输。溶液pH值对GO在石灰岩中的传输影响较小,质量回收率范围为40.3%至51.7%。总体而言,在所测试的条件下,溶液pH值、HA浓度的降低以及溶液离子强度的增加都会降低GO在石灰岩介质中的迁移率。这些结果表明,环境条件和介质特性在控制GO在多孔介质中的归宿和传输方面都起着重要作用。应用单点位动力学沉积模型来描述GO与石灰岩介质之间的相互作用,模型模拟结果与观测实验数据拟合得非常好。由于石灰岩是地下含水层介质的重要组成部分,本研究结果阐明了控制GO颗粒在石灰岩介质中归宿的关键因素和过程,可为预测和评估GO在地下水环境中的风险提供依据。