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EXPERIMENTAL AND THEORETICAL INVESTIGATION OF LNAPL MOVEMENT IN STRATIFIED MEDIA DURING SOIL REMEDIATION

机译:土壤修复过程中分层介质中LNAPL运动的实验和理论研究

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The saturation distribution and clean up efficiency of light non-aqueous phase liquid (LNAPL) in the strata beneath the earth has been the subject of many studies. Better understanding of LNAPL infiltration into layered soil is important for the effective design of remediation strategies. The objective of this study was to simulate LNAPL movement in homogenous and stratified porous media using gravity assisted inert gas injection (GAIGI) process as a cleaning technique. We used homogeneous and layered sandpacked transparent models that allows for visual observation of LNAPL movement in order to study LNAPL redistribution in a layered porous medium. Pore volume, porosity, absolute permeability, connate water saturation, and oil saturation of the models were determined experimentally. Seasonal water table movement and contaminated zone were established and then, under GAIGI process, clean up efficiency was determined. The downward displacement of LNAPL by gas drive resulted in very high LNAPL clean up efficiency. Using the contaminant production history in the homogeneous model, the LNAPL relative permeability was calculated and the results were extended to layered media. The numerical multi-phase flow model in porous media was validated with regard to the experimental results. This model is able to adequately reproduce the experimental LNAPL saturation profile and clean up efficiency.
机译:地下地层中轻非水相液体(LNAPL)的饱和度分布和净化效率已成为许多研究的主题。更好地了解LNAPL渗透到层状土壤中对于有效设计补救策略很重要。这项研究的目的是使用重力辅助惰性气体注入(GAIGI)工艺作为清洁技术来模拟LNAPL在均质和分层多孔介质中的运动。为了研究LNAPL在分层多孔介质中的重新分布,我们使用了均质且分层的沙袋状透明模型,该模型可以直观观察LNAPL的运动。实验确定了模型的孔体积,孔隙率,绝对渗透率,原生水饱和度和油饱和度。建立季节性的地下水位移动和污染区,然后在GAIGI过程中确定清理效率。气体驱动使LNAPL向下移动,导致LNAPL的净化效率非常高。使用均质模型中的污染物产生历史,可以计算LNAPL相对渗透率,并将结果扩展到分层介质。根据实验结果验证了多孔介质中多相流的数值模型。该模型能够充分再现实验性LNAPL饱和度分布图和清理效率。

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