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How Big is My Rock Toe? A Geophysical Success Story

机译:我的摇滚脚趾有多大?地球物理的成功故事

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The size and configuration of an existing rock toe was a key piece of information required for evaluating possible dam safety modifications for Rampart Dam, Colorado. Geophysical investigations consisting of six Electric Resistivity Imaging (ERI) survey lines were successfully used to define the extent of the rock toe. Seven drill holes were completed to confirm the results of the ERI survey. The geophysical investigations reduced the total cost of the field investigations and limited the extent of intrusive investigations. Rampart Dam, an approximately 250-ft high zoned embankment dam, is classified as a high hazard structure. The facility is owned, operated, and maintained by Colorado Springs Utilities (Utilities). Rampart Dam provides terminal water supply storage for the Utilities' system and is a critical component of the water supply system. The rock toe is located at the downstream toe of the dam. Seepage has exited the downstream face of the embankment above the rock toe since original construction of the dam. Concerns regarding the observed seepage at this location are: 1) unfiltered seepage exiting the downstream slope above the rock toe, and 2) apparent lack of filters between the embankment shell (Zone 2) material and the rock toe. Seepage gradients within the dam appear to be low, seepage conditions have been consistent for a long period of time, and no evidence of internal erosion has been reported. However, seepage is exiting the dam at unfiltered locations, so the possibility of development of internal erosion cannot be ruled out. Utilities desired to evaluate alternatives to address the seepage concerns. The rock toe was built as part of the original construction completed in 1969, and the size and configuration of the rock toe was not clear, based on information from design and construction and previous subsurface investigations. It became clear that the size and configuration of the rock toe could limit the extent of the downstream section of the dam that could be practically excavated, which in turn affected the feasibility of some modification alternatives. Field investigations to define the extent and configuration of the rock toe became a priority.
机译:现有岩石脚趾的尺寸和配置是评估卢布拉多大坝,科罗拉多州的可能的水坝安全修改所需的关键信息。由六种电阻率成像(ERI)调查线组成的地球物理调查成功地用于定义岩石脚趾的范围。完成了七个钻孔以确认ERI调查结果。地球物理调查减少了现场调查的总成本,并限制了侵入性调查的程度。 RAMPART大坝,大约250英尺高划线大坝,被归类为高危险结构。该设施由Colorado Springs Utilities(公用事业)拥有,操作和维护。 RAMPART DAM为公用事业系统提供终端供水存储,是供水系统的关键组成部分。岩石脚趾位于大坝的下游脚趾。自原始建筑以来,渗漏从岩石脚趾上方的堤防下游面孔离开。对观察到的渗漏的担忧是:1)未过滤的渗流离开岩石脚趾上方的下游斜坡,2)在堤防壳(区域2)材料和岩石脚趾之间表观缺乏过滤器。大坝内的渗流梯度看起来很低,渗流条件一直一致一段时间,没有报道内部侵蚀的证据。然而,渗漏是在未过滤的位置离开大坝,因此无法排除内部侵蚀的可能性。希望评估解决渗漏问题的替代品的实用程序。岩石脚趾是由1969年完成的原始建筑的一部分建造的,而岩石脚趾的尺寸和配置尚不清楚,基于设计和施工和以前的地下调查的信息。很明显,岩石脚趾的尺寸和配置可能会限制水坝的下游部分的程度,这些可能是实际挖掘的,这反过来影响了一些修改替代方案的可行性。实地调查定义岩石脚趾的范围和配置成为优先事项。

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