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Merging of borehole data for federal inter-state 3D-modelling in the Upper-Rhine-Graben

机译:在莱茵 - Graben中联邦州间3D建模的钻孔数据的合并

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摘要

Heterogeneous data structures in federal inter-state projects for 3D geological and/or groundwater modelling often face significant challenges. To address and overcome these challenges, three cross-border areas in Germany have been chosen for apilot study. Geologically, the areas are located in the Upper Rhine Graben and the Hanau-Seligenstadt Basin. Borehole data provided by the geological surveys have been compared and synthesized according to technical and content-related criteria. Synthesized data were then parameterized with defined classes of hydraulic conductivity and interpolated in 3D space, aiming to spatially describe the hydraulic conductivity. In addition, for one subsection, borehole data were interpreted within acommon lithostratigraphic context for modelling Quaternary horizons across federal state borders. Asemi-automated synthesis of petrographic information worked for most of the geological layers. Results reveal the occurrence of high permeability layers in the first 40meters below ground surface and low permeability layers in the following 30meters. The permeability model correlates well with modelled Quaternary horizons.
机译:用于3D地质和地下水建模的联邦州间项目中的异构数据结构经常面临重大挑战。为了解决并克服这些挑战,选择了德国的三个跨境地区,为Apilot研究选择了。地质上,该地区位于莱茵河上部莱茵河和哈国塞格纳斯塔特盆地。通过地质调查提供的钻孔数据已经进行了比较和合成,根据技术和内容相关的标准。然后,合成数据通过定义的液压导电性进行参数化,并在3D空间中插值,旨在在空间上描述液压导电性。此外,对于一个小节,钻孔数据被解释在Acommon LithoStraphicic语境中,用于在联邦国家边界跨越季度视野。宇宙 - 自动化岩体信息的综合,适用于大多数地质层。结果揭示了在接地表面以下的前40米中的高渗透层的发生,下面的30米处的低渗透层。渗透性模型与建模的第四纪视野相关联。

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