首页> 外文会议>Association of State Dam Safety Officials annual conference >3d Geologic Modeling and Probabilistic Stability Analyses Support a Rock Face Stabilization Project at Boundary Dam, Pend Oreille River, Washington State
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3d Geologic Modeling and Probabilistic Stability Analyses Support a Rock Face Stabilization Project at Boundary Dam, Pend Oreille River, Washington State

机译:3D地质建模和概率稳定性分析支持山上稳定项目,在华盛顿州的Pend Oreille River,Pend Oreille River

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Seattle City Light's Boundary Dam is a 340-foot high double curvature concrete arch in a steep, narrow canyon on the Pend Oreille River in northeastern Washington. Original site explorations included over 100 borings and exploratory adits to support design and construction of the dam, the large underground powerhouse, the forebay, penstocks, draft tubes and extensive access and diversion tunnels. Recent work at the dam includes laser scanning of both aboveground area and underground works. Rock bolting of large potential slide blocks and underground excavations was completed both during construction and later. However, continued concerns over the stability of the steep rock face on the right abutment and the lack of an integrated understanding of the site geology prompted development of a computer-based, 3D geologic model. The model integrates the laser scans with the original exploratory borings, geologic maps, and information gleaned from an extensive library of construction photographs. The model allows a site-wide, 3D visualization of the spatial relationships of the rock types, through-going joint planes, topography, and the numerous project excavations and constructed features. The right abutment was given specific attention, and the geometries and possible release planes for large, potentially removable blocks near the dam were defined in the model. Kinematic analyses demonstrated little risk to the dam. However, the work did lead to concerns regarding the stability of a pier supporting the access bridge from the dam face to the right abutment. Field work and probabilistic stability analyses led to the decision to stabilize the pier foundation.
机译:西雅图城市灯的边界大坝是一家340英尺高的双曲率混凝土拱,在华盛顿东北部的PEND OREILLE河上的陡峭狭窄的峡谷。原始网站探索包括100多个Borings和探索性探索,以支持大坝的设计和建造,大型地下电力房,前沟,口碑,拔出管道和广泛的进入和转移隧道。最近在大坝的工作包括在地下区域和地下工作的激光扫描。在施工期间,楼上完成了大潜在滑块和地下挖掘的岩石螺栓。然而,对陡峭的岩石面对右基台的稳定性以及对网站地质的综合理解缺乏担忧,促使基于计算机的3D地质模型的发展。该模型将激光扫描与原始探索性Borings,地质地图和信息从广泛的施工图书馆获取信息集成。该模型允许岩石类型的空间关系,穿越平面,地形和众多项目挖掘和构造特征的站点宽的3D可视化。正确的邻接是特别的关注,并且在模型中定义了大坝附近的大型可能可移动块的几何和可能的释放平面。运动学分析对大坝的风险很少。然而,该工作确实导致关于码头的稳定性的担忧,该码头支持从大坝面向正确的邻接。现场工作和概率稳定性分析导致决定稳定码头基础。

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