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Seismic Stability Analysis and Risk Assessment of Lake Elmer Thomas Dam

机译:埃尔默托马斯大坝湖的地震稳定性分析与风险评估

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Lake Elmer Thomas Dam is a 421-foot-long, roller-compacted concrete (RCC) gravity dam on Little Medicine Creek in Comanche County, Oklahoma. The dam is only 0.5 miles upstream of the town of Medicine Park and impounds a reservoir with a maximum storage capacity of 11,800 acre-feet. With a maximum height of approximately 113 feet, Lake Elmer Thomas Dam is classified as a high hazard dam. The RCC dam is founded on massive Mount Scott Granite, approximately 3.7 miles (6 km) from the Meers fault at its closest mapped trace. A site-specific seismic hazard assessment, completed in 2015, indicated that the recommended Safety Evaluation Earthquake (SEE), with a return period of 10,000 years, and the deterministic Maximum Credible Earthquake (MCE) would result in peak ground accelerations (PGAs) at the site of 1.22 g and 2.08 g, respectively. Both of these PGAs are significantly greater than the PGA of 0.8 g used in the pseudo-static analysis of the dam during original design and subsequent stability evaluations. To address concerns regarding the stability of the dam for the larger ground motions, an updated seismic stability evaluation and quantitative risk analysis of the Lake Elmer Thomas Dam were performed. The seismic stability evaluation was performed using a two-dimensional pseudo-dynamic analysis of the dam for the SEE and MCE, and updated RCC and foundation strength parameters based on a statistical analysis of data from the original design and construction. Due to the large population at risk, the risk analysis used the results from the seismic stability evaluation and additional sensitivity studies to extrapolate the response of the dam to even larger ground motions. The results of the risk analysis indicated that the mean estimate for the annualized loss of life related to the potential failure of Lake Elmer Thomas Dam falls below the Bureau of Reclamation's guideline for increasing justification for risk reduction actions, and no further work or studies were recommended. Plans for careful visual inspection of the dam and review of monitoring data following ground motions felt in the area were developed.
机译:埃尔默湖托马斯大坝是一个421英尺长的滚筒压实的混凝土(RCC)在俄克拉荷马州康曼县小医学溪上的重力坝。大坝仅在医学镇上游0.5英里,储存储层,最大储存能力为11800英亩。埃尔默湖托马斯大坝占地面积大约113英尺的高度。 RCC大坝建于大山斯科特花岗岩,大约3.7英里(6公里),距离Meers Fault最近的映射跟踪。在2015年完成的场地特异性地震危险评估表明,推荐的安全评估地震(见),返回期限为10,000年,而确定性最大可信地震(MCE)将导致峰会地面加速(PGA)分别为1.22克和2.08克的部位。这两个PGA在原始设计期间和随后的稳定性评估期间,在大坝的伪静态分析中使用的0.8g的PGA显着大于0.8g。为了满足关于大坝稳定性的较大地面运动的担忧,进行了伊尔默托马斯大坝的更新的地震稳定性评估和定量风险分析。基于来自原始设计和施工的数据的统计分析,使用大坝的二维伪动态分析进行地震稳定性评估,以及更新RCC和基础强度参数。由于风险的巨大群体,风险分析使用了地震稳定性评估的结果和额外的敏感性研究,以将大坝的反应推断到甚至更大的地面运动。风险分析结果表明,与伊尔默托马斯大坝湖潜在失败相关的年化生命损失的平均估计低于填写局的局面,以提高风险降低行动的理由,并没有建议进一步的工作或研究。制定了仔细视觉检查水坝的计划,并开发了该地区的地面运动后监测数据的审查。

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