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Engineering Properties Determination of In-Situ Glacial Till and Lacustrine Silt associated with Remediation of Deep Seated Abutment Movement Downstream of Nesbitt Dam

机译:奈斯比特大坝下游深基台移动修复的原位冰川耕作和湖相淤泥的工程特性确定

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Nesbitt Dam is a composite earth-fill embankment with stone masonry corewall, non-overflow and spillway section. Historical survey data indicate that thedownstream hillside and right abutment has been subjected to movement over a60 year period from 1920 to 1980s. Inclinometers established during a 2007subsurface investigation depicted 12.7 millimeters (0.5 inches) of movement within alacustrine silt stratum at a depth of approximately 30 meters (100 feet) six monthsafter installation. This paper presents the procedures and analyses used by GannettFleming to identify, model, and design a remedial solution to limit future hillsideinstability. This paper focuses on the extensive laboratory testing program conductedon the lacustrine silt and adjacent strata to thoroughly establish the engineeringproperties of site soils.
机译:内斯比特大坝是具有砌石芯的复合土方路堤 墙,非溢流和溢洪道部分。历史调查数据表明 下游山坡和右基台已经过 从1920年到1980年代的60年。在2007年建立的测斜仪 地下调查描绘了12.7毫米(0.5英寸)的运动范围。 湖泊淤泥层,深度约30米(100英尺),六个月 安装后。本文介绍了Gannett使用的过程和分析 弗莱明(Fleming)识别,建模和设计补救解决方案,以限制未来的山坡 不稳定。本文重点介绍了广泛的实验室测试计划 在湖粉质及邻近地层上彻底建立工程 场地土壤的特性。

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