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A study of dense nonaqueous phase liquid infiltration in saturated porous media: Centrifuge simulations and similitude analysis.

机译:饱和多孔介质中稠密非水相液体渗透的研究:离心模拟和相似性分析。

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The problem of dense nonaqueous phase liquid (DNAPL) migration in the subsurface was studied with the aid of similitude analysis, analytical solutions, and physical simulations. The scaling laws of two-phase transport were modified to better describe DNAPL migration under constant and falling head conditions. A semi-analytical solution was developed which gives the velocity and location of the DNAPL front and a criterion that describes the mobility condition of the DNAPL front. Several column experiments conducted under 1-g and using different soils and three DNAPLs spanning a wide range of DNAPL properties agreed reasonably well with the model predictions and verified the modified scaling laws.;Two-dimensional simulations of DNAPL infiltration in saturated porous media were performed in the geotechnical centrifuge to: (a) assess current conceptual models, (b) study the mobility trends of DNAPLs in different soil models, and (c) provide data for numerical code validation. Contrary to current conceptual models, the centrifuge simulations showed that low density DNAPLs may reach a halt without encountering a capillary barrier, at DNAPL saturations much higher than residual. In homogeneous soil models, DNAPLs with low density and high viscosity penetrated approximately equally in both dimensions. On the other hand, DNAPLs with high density and low viscosity showed increased mobility in the vertical direction with little lateral spreading. In layered soil models, DNAPL movement was dominated by lateral spreading in the coarse layers. In compacted clays, DNAPL migration occurred primarily in the macroscopic features of the clay such as cracks and interclod voids.
机译:借助相似度分析,解析解和物理模拟,研究了地下非稠相液体(DNAPL)迁移的问题。修改了两相传输的定标律,以更好地描述恒定和下降水头条件下的DNAPL迁移。开发了一种半分析解决方案,它给出了DNAPL前沿的速度和位置以及描述DNAPL前沿的迁移条件的标准。在1-g下使用不同土壤和三种涵盖广泛DNAPL性质的DNAPL进行的几项柱实验与模型预测相当吻合,并验证了修正的比例定律。;进行了饱和多孔介质中DNAPL渗透的二维模拟在岩土离心机中:(a)评估当前的概念模型,(b)研究不同土壤模型中DNAPLs的迁移趋势,以及(c)为数字代码验证提供数据。与当前的概念模型相反,离心机模拟显示,低密度DNAPLs可能会停下来而不会遇到毛细屏障,而DNAPL的饱和度要远高于残留物。在均质土壤模型中,低密度和高粘度的DNAPL在两个维度上的渗透率大致相等。另一方面,具有高密度和低粘度的DNAPL在垂直方向上显示出增加的迁移率,而横向扩展很小。在分层土壤模型中,DNAPL的移动主要由在粗层中的横向扩展所决定。在压实的粘土中,DNAPL迁移主要发生在粘土的宏观特征中,例如裂缝和空隙间空隙。

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