首页> 外文会议>XIVth International Conference on Computational Methods in Water Resources (CMWR XIV), Jun 23-28, 2002, Delft, The Netherlands >Investigation of a tensor renormalization method to determine the effective conductivity of heterogeneous subsoils
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Investigation of a tensor renormalization method to determine the effective conductivity of heterogeneous subsoils

机译:张量重归一化方法确定异质土有效电导率的研究

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For consultancy in civil and environmental engineering there is a need for a fast yet sufficiently accurate estimate of the hydraulic conductivity field of always heterogeneous subsoils. Therefore, a simple semi-analytical upscale procedure using the renormalization method is investigated to determine the hydraulic conductivity of heterogeneous soil with a schematized sedimentary structure. The investigated procedure is faster than traditional numerical upscaling methods in that the small-scale conductivity fields is scaled up analytically to the scale of a unit cell for application in for example finite element modelling. The upscaling of various unit cells (with statistical characteristics of the small-scale structure) to the desired scale is performed with two tensor renormalization methods. Both methods have been tested for several analytical configurations.
机译:为了在土木和环境工程中提供咨询,需要快速而足够准确地估计总是非均质地下土的水力传导率场。因此,研究了一种使用重归一化方法的简单的半解析高级程序,以确定具有示意性沉积结构的非均质土壤的水力传导率。与传统的数值放大方法相比,所研究的过程更快,因为小尺度电导率场可解析地放大到单位晶格的尺度,以用于例如有限元建模。使用两种张量重归一化方法将各种单位单元(具有小规模结构的统计特征)放大到所需规模。两种方法都经过了几种分析配置的测试。

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