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为华盛顿州Pend Oreille河边界大坝的岩壁稳定项目提供了支持

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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:西雅图城市之光的边界水坝是一个340英尺高的双曲率混凝土拱门,位于华盛顿东北部的彭德·奥雷河上的陡峭狭窄峡谷中。最初的现场勘探包括100多个钻孔和探洞,以支持大坝,大型地下动力站,前湾,压力管道,引水管以及广泛的进水和改道隧道的设计和建设。大坝最近的工作包括对地上和地下工程进行激光扫描。大型潜在滑块和地下挖掘的岩石锚固在施工期间及以后均已完成。但是,由于人们对右侧基台上陡峭岩壁的稳定性的持续关注,以及对现场地质状况缺乏全面了解,促使开发了基于计算机的3D地质模型。该模型将激光扫描与原始探索性钻孔,地质图以及从广泛的建筑图片库中收集的信息集成在一起。该模型可以在整个站点范围内以3D形式显示岩石类型,贯穿的联合平面,地形以及众多项目开挖和构造特征的空间关系。右侧基台受到了特别的关注,并且在模型中定义了大坝附近潜在的大型可移动块的几何形状和可能的释放平面。运动学分析表明,对大坝的风险很小。但是,这项工作的确引起了人们对从水坝面到右桥墩的支撑通行桥的墩墩稳定性的担忧。现场工作和概率稳定性分析导致了稳定墩基础的决定。

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