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Inverse approaches with lithologic information for a regional groundwater system in southwest Kansas

机译:堪萨斯州西南部区域地下水系统的岩性信息反演

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摘要

Two practical approaches incorporating lithologic information for groundwater modeling calibration are presented to estimate distributed, cell-based hydraulic conductivity. The first approach is to estimate optimal hydraulic conductivities for geological materials by incorporating thickness distribution of materials into inverse modeling. In the second approach, residuals for the groundwater model solution are minimized according to a globalized Newton method with the aid of a Geographic Information System (GIS) to calculate a cell-wise distribution of hydraulic conductivity. Both approaches honor geologic data and were effective in characterizing the heterogeneity of a regional groundwater modeling system in southwest Kansas. (c) 2005 Elsevier Ltd All fights reserved.
机译:提出了两种结合岩性信息进行地下水建模校准的实用方法,以估算基于单元的分布式水力传导率。第一种方法是通过将材料的厚度分布纳入反演模型来估算地质材料的最佳水力传导率。在第二种方法中,借助全球化的牛顿法,借助地理信息系统(GIS)来最小化地下水模型解决方案的残差,以计算水力传导率的单元分布。两种方法都尊重地质数据,并有效地表征了堪萨斯州西南部区域地下水建模系统的非均质性。 (c)2005 Elsevier Ltd版权所有。

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