首页> 外文期刊>Advances in Water Resources >Determination of the diffusivity, dispersion, skewness and kurtosis in heterogeneous porous flow. Part Ⅰ: Analytical solutions with the extended method of moments.
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Determination of the diffusivity, dispersion, skewness and kurtosis in heterogeneous porous flow. Part Ⅰ: Analytical solutions with the extended method of moments.

机译:测定非均质多孔流中的扩散率,色散,偏度和峰度。第一部分:扩展矩量法的解析解。

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The extended method of moments (EMM) is elaborated in recursive algorithmic form for the prediction of the effective diffusivity, the Taylor dispersion dyadic and the associated longitudinal high-order coefficients in mean-concentration profiles and residence-time distributions. The method applies in any streamwise-periodic stationary d-dimensional velocity field resolved in the piecewise continuous heterogeneous porosity field. It is demonstrated that EMM reduces to the method of moments and the volume-averaging formulation in microscopic velocity field and homogeneous soil, respectively. The EMM simultaneously constructs two systems of moments, the spatial and the temporal, without resorting to solving of the high-order upscaled PDE. At the same time, the EMM is supported with the reconstruction of distribution from its moments, allowing to visualize the deviation from the classical ADE solution. The EMM can be handled by any linear advection-diffusion solver with explicit mass-source and diffusive-flux jump condition on the solid boundary and permeable interface. The prediction of the first four moments is decisive in the optimization of the dispersion, asymmetry, peakedness and heavy-tails of the solute distributions, through an adequate design of the composite materials, wetlands, chemical devices or oil recovery. The symbolic solutions for dispersion, skewness and kurtosis are constructed in basic configurations: diffusion process and Darcy flow through two porous blocks in "series", straight and radial Poiseuille flow, porous flow governed by the Stokes-Brinkman-Darcy channel equation and a fracture surrounded by penetrable diffusive matrix or embedded in porous flow. We examine the moments dependency upon porosity contrast, aspect ratio, Peclet and Darcy numbers, but also for their response on the effective Brinkman viscosity applied in flow modeling. Two numerical Lattice Boltzmann algorithms, a direct solver of the microscopic ADE in heterogeneous structure and a novel scheme for EMM numerical formulation, are called for validation of the constructed analytical predictions.
机译:扩展的矩量法(EMM)以递归算法形式进行了详细说明,以预测平均浓度分布和停留时间分布中的有效扩散率,泰勒色散二阶以及相关的纵向高阶系数。该方法适用于在分段连续非均质孔隙度场中解析的任何流周期周期性d维速度场。结果表明,EMM在微观速度场和均质土中分别简化为矩量法和体积平均法。 EMM同时构建两个矩系统,即空间和时间矩,而无需求助于高阶放大的PDE。同时,EMM还支持从其瞬间重新分布,从而可视化与经典ADE解决方案的偏差。 EMM可以通过任何在固体边界和渗透性界面上具有显式质量源和扩散通量跳跃条件的线性对流扩散求解器来处理。通过适当设计复合材料,湿地,化学装置或采油,对前四个矩的预测对于溶质分布的分散性,不对称性,峰度和重尾的优化起决定性作用。色散,偏度和峰度的象征性解决方案以以下基本构造构成:扩散过程和达西流经“系列”中的两个多孔块,直线和径向Poiseuille流,由Stokes-Brinkman-Darcy通道方程控制的多孔流和裂缝被可渗透的扩散基质包围或嵌入多孔流中。我们检查了矩对孔隙率对比,纵横比,Peclet和Darcy数的依赖性,还研究了它们对流动建模中有效Brinkman粘度的响应。为了验证所构造的分析预测,需要两种数值Lattice Boltzmann算法,异质结构中微观ADE的直接求解器和EMM数值公式化的新方案。

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