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Multidimensional validation of a numerical model for simulating a DNAPL release in heterogeneous porous media

机译:用于模拟非均质多孔介质中DNAPL释放的数值模型的多维验证

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摘要

A fixed-volume release of 1,2-DCE, tracked in space and time with a light transmission/image analysis system, provided a data set for the infiltration, redistribution, and immobilisation of a dense non-aqueous phase liquid (DNAPL) in a heterogeneous porous medium. The two-dimensional bench scale flow cell was packed with a spatially correlated, random heterogeneous distribution of six sand types. In order to provide the necessary modelling parameters, detailed constitutive relationships were measured at the local scale for the six sands. These experiments revealed that nonwetting phase (NWP) relative permeability-saturation (k_(rN)-S_W) relationships are strongly correlated to sand type. Trends in the best-fit k_(rN)-S_w parameters reflected a positive correlation between mean grain diameter and the maximum NWP relative permeability, k_(rN)~(max). Multiphase flow simulations of the bench scale experiment best reproduced the experimental observations, producing excellent matches in both time and space, when the measured, correlated local scale k_(rN)-S_W relationships were employed.
机译:用光透射/图像分析系统在空间和时间上跟踪固定体积的1,2-DCE释放,为浓密非水相液体(DNAPL)的渗透,重新分布和固定提供了数据集。异质多孔介质。二维台式规模流动池充满了六种砂类型的空间相关,随机异质分布。为了提供必要的建模参数,对六种砂子在局部尺度上测量了详细的本构关系。这些实验表明,非润湿相(NWP)相对渗透率-饱和度(k_(rN)-S_W)关系与砂类型密切相关。最佳拟合k_(rN)-S_w参数的趋势反映了平均粒径与最大NWP相对磁导率k_(rN)〜(max)之间呈正相关。台式规模实验的多相流模拟最好地重现了实验观察结果,当采用测量的,相关的局部尺度k_(rN)-S_W关系时,在时间和空间上都产生了出色的匹配。

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