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High-resolution experiments on chemical oxidation of DNAPL in variable-aperture fractures

机译:可变孔径骨折中DNAPL化学氧化的高分辨率实验

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摘要

Chemical oxidation of dense nonaqueous-phase liquids (DNAPLs) by permanganate has emerged as an effective remediation strategy in fractured rock. We present high-resolution experimental investigations in transparent analog variable-aperture fractures to improve understanding of chemical oxidation of residual entrapped trichloroethylene (TCE) in fractures. Four experiments were performed with different permanganate concentrations, flow rates, and initial TCE phase geometry. The initial aperture field and evolving entrapped-phase geometry were quantified for each experiment. The integrated mass transfer rate from the TCE phase for all experiments exhibited three time regimes: an early-time regime with slower mass transfer rates limited by low specific interfacial area; an intermediate-time regime with higher mass transfer rates resulting from breakup of large TCE blobs, which greatly increases specific interfacial area; and a late-time regime with low mass transfer rates due to the deposition of MnO2 precipitates. In two experiments, mass balance analyses suggested that TCE mass removal rates exceeded the maximum upper bound mass removal rates derived by assuming that oxidation and dissolution are the only mechanisms for TCE mass removal. We propose incomplete oxidation by permanganate and TCE solubility enhancement by intermediate reaction products as potential mechanisms to explain this behavior. We also speculate that some intermediate reaction products with surfactant-like properties may play a role in lowering the TCE-water interfacial tension, thus causing breakup of large TCE blobs. Our quantitative experimental measurements will be useful in the context of developing accurate computational models for chemical oxidation of TCE in fractures.
机译:高锰酸盐对致密非水相液体(DNAPLs)的化学氧化已经成为裂隙岩石中一种有效的修复策略。我们目前在透明模拟可变孔径裂缝中进行高分辨率实验研究,以增进对裂缝中残留的三氯乙烯(TCE)残留化学氧化的理解。用不同的高锰酸盐浓度,流速和初始TCE相几何形状进行了四个实验。对于每个实验,对初始孔径场和演化的陷相几何结构进行了量化。对于所有实验,TCE阶段的综合传质速率均表现出三种时间模式:一种传质速率较慢的早期模式,受较低的比界面面积限制;由于较大的TCE斑点破裂而导致的传质速率较高的中间时间体制,这大大增加了比界面面积;以及由于MnO2沉淀物的沉积而使传质速率低的后期方案。在两个实验中,质量平衡分析表明,TCE的质量去除率超过了最大上限质量去除率,该假设是假设氧化和溶解是TCE去除质量的唯一机制。我们提出通过高锰酸盐的不完全氧化和通过中间反应产物的三氯乙烯(TCE)溶解度的增强作为解释这种行为的潜在机制。我们还推测某些具有表面活性剂性质的中间反应产物可能在降低TCE-水界面张力,从而导致大的TCE斑点破裂方面起作用。我们的定量实验测量结果将为开发裂缝中TCE的化学氧化的精确计算模型提供帮助。

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