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Geologic site characterization for deep nuclear waste disposal in fractured rock based on 3K data visualization

机译:基于3K数据可视化的裂隙岩深部核废料处置地质部位表征

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Three-dimensional (3D) visualization of data is anessential step in the development of descriptive hydrologic androck-mechanical models of fractured rock systems. Data includesgeological properties, rock mechanical properties and hydraulicresponses. The 3K visualization approach is applied tocharacterizing a hypothetical site for a high-level nuclear wasterepository located at 500m depth in granitoids of the trans-Scandinavian igneous belt (1.6-1.8 Ga old). The study is based onsite-specific data at the Aspo Hard Rock Laboratory (HRL) onthe southeastern coast of Sweden. The data are extensive andspatially complex and are based on surface information, as wellas a large number of boreholes penetrating up to 1000m. At thissite, fracture and fracture zones control both groundwater flowand mechanical stability. Structures are found within a 2×2×1 kmdeep model block representing the site. 3Dlocations of fracturesand fracture zones are hypothesized based on surface andsubsurface geological geophysical information, includingborehole radar. This results in a 3D geological model structure of the site.
机译:数据的三维(3D)可视化是裂缝性岩石系统的描述性水文和岩石力学模型开发的重要步骤。数据包括地质性质,岩石力学性质和水力响应。 3K可视化方法用于表征一个假想的地点,该地点位于反斯堪的纳维亚火成岩带(1.6-1.8 Ga年代)的花岗岩类中位于500m深度的高级核废料仓库。这项研究基于瑞典东南沿海Aspo硬岩实验室(HRL)的现场特定数据。数据是广泛且空间复杂的,并且基于地表信息以及大量贯穿1000m的井眼。在该位置,裂缝和裂缝带控制着地下水的流量和机械稳定性。在代表该站点的2×2×1 kmd深模型块中找到结构。 3根据地表和地下地质地球物理信息(包括钻孔雷达),假设裂缝和裂缝区域的位置。这将导致该站点的3D地质模型结构。

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