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Transport of graphene oxide nanoparticles in saturated kaolinite- and goethite-coated sand columns: effects of low-molecular-weight organic acids

机译:饱和高岭石和甲酸酯涂层砂柱中石墨烯氧化物纳米粒子的运输:低分子量有机酸的影响

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The effects of low-molecular-weight organic acids (LMWOAs) on the transport of graphene oxide nanoparticles in saturated kaolinite- and goethite-coated sand columns were studied. Acetic acid, glycolic acid, malonic acid, and tartaric acid were chosen in the experiments. LMWOAs enhanced the mobility of GO by electrostatic/steric repulsion. In addition, they competed with GO for limited deposition sites on grain surfaces. The effects of organic acids on the transport of GO strongly depended on organic acid species. In general, the transport enhancement effects followed the order of tartaric acid > malonic acid > glycolic acid > acetic acid; this difference may be related to the number and type of functional groups of organic acids. Different LMWOAs enhanced the transport of GO in goethite-coated sand to a larger extent than did in kaolinite-coated sand under the test conditions; this was likely related to the differences of physicochemical characteristics between goethite and kaolinite. Organic acids significantly inhibited the deposition of GO at 0.5 mM Ca2+; this was possible that Ca2+ enhanced adsorption of organic acids by complexing with the surface O-functionalities of both LMWOAs and sand grain. Consequently, more organic acid molecules competed with GO for deposition sites on grain surfaces. Additionally, a two-site transport model was used to fit the transport data. Our findings have important implications for the understanding of the deposition and fate of GO in soil especially in rhizosphere environments where various low-molecular-weight organic acids are active.
机译:研究了低分子量有机酸(LMWOAs)对饱和高岭石和乙腈涂层砂柱中石墨烯纳米颗粒的运输的影响。在实验中选择乙酸,乙醇酸,丙二酸和酒石酸。 LMWOAS通过静电/空间排斥来增强了Go的移动性。此外,他们竞争谷物表面上的有限沉积网站。有机酸对持续运输的影响强烈依赖于有机酸物种。一般来说,运输增强效果遵循酒石酸>丙二酸>乙酸>乙酸;这种差异可能与有机酸的官能团的数量和类型有关。不同的LMWOAS增强了在粘散的砂岩中的运输到更大程度上,而不是在试验条件下在高岭石涂层砂中进行;这可能与鹅料和高岭石之间的物理化学特征的差异有关。有机酸显着抑制了0.5mM Ca2 +的沉积;通过与Lmwoas和砂粒的表面o函数络合,Ca2 +通过络合而增强了有机酸的吸附。因此,更多有机酸分子与晶粒表面上的沉积位点竞争。另外,使用双站点传输模型来符合传输数据。我们的研究结果对理解在土壤中的沉积和命运的理解中具有重要意义,特别是在各种低分子量有机酸活性的根际环境中。

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