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Modelling groundwater exchange between the hydrogeological units of Erftscholle, Rurscholle, and Venloer Scholle by coupling large scale groundwater models

机译:通过耦合大型地下水模型对Erftscholle,Rurscholle和Venloer Scholle的水文地质单位之间的地下水交换进行建模

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摘要

three large-scale groundwater models were developed for the purpose of water resources management during open pit mining activities. the area of interest is a part of the Lower Rhine embayment, the modelling areas cover the geological units ( blocks) of the Venlo terrain, the Rur terrain and the Erft terrain, which are separated by geologic faults. the groundwater interchange between the three blocks is modelled by setting shared boundary conditions at which the interchange was equilibrated in an iterative process. by coupling the three models numerically using finite beam elements, the process of adjusting the boundary conditions can be avoided. the beam elements only model the interchange paths between the blocks, but not the block-separating faults themselves. therefore, this method is appropriate for large-scale modelling, because arbitrary interchange paths can be modelled without describing the faults in detail.
机译:为了在露天采矿活动中进行水资源管理,开发了三个大型地下水模型。感兴趣的区域是下莱茵河保护区的一部分,建模区域覆盖了由地质断层隔开的芬洛地形,鲁尔地形和厄尔夫特地形的地质单元(块)。通过设置共享边界条件来模拟三个区块之间的地下水交换,在迭代过程中平衡交换条件。通过使用有限梁单元数值耦合三个模型,可以避免调整边界条件的过程。梁单元仅模拟块之间的交换路径,而不模拟块分离断层本身。因此,该方法适用于大规模建模,因为可以对任意交换路径进行建模而无需详细描述故障。

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