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Finite-element analysis of the failure and reconstruction of the main dam embankment at Abberton Reservoir, Essex, UK

机译:英国艾塞克斯阿伯顿水库主坝路堤破坏与重建的有限元分析

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An existing 15·5 m high main dam embankment at Abberton Reservoir in Essex was completed in August 1938, since when its performance has been satisfactory. However, the upstream embankment shoulder of the original dam suffered a deep-seated failure through its foundation towards the end of construction in July 1937, 9 days before a similar and well-known failure occurred at Chingford Reservoir in close proximity to Abberton. Whereas the failure at Chingford became an important case in the history of soil mechanics through the involvement of Karl Terzaghi and marked one of the first applications of modern soil mechanics principles, the failure at Abberton has remained largely unknown, until recently when raising of the existing dam started to be considered. This paper describes advanced finite-element analyses which were carried out to investigate the failure of the original dam at Abberton and the stability of the existing main dam. The parameters used in the constitutive models were derived on the basis of the available site investigations and laboratory testing and on experience in the back-analysis of other failures in London Clay. The analyses demonstrated that the upstream shoulder of the original embankment failed through the mechanism of progressive failure, which involved the top of the stiff plastic London Clay rather than the overlying alluvium in the foundation. The relatively rapid rate of embankment filling, achieved by using modern earth-moving equipment, contributed significantly to the original dam failure. The analyses also demonstrated satisfactory behaviour of the existing dam during reconstruction, the first impounding and in the long term, with its response being similar to that observed. Thus the constitutive models used and parameters derived were successfully calibrated against the observed behaviour of both the original and existing main dams at Abberton, and could be used in predicting the behaviour of the dam during and after its proposed raising.
机译:自1938年8月以来,埃塞克斯郡阿伯顿水库现存的15·5 m高的主坝路堤竣工,当时其性能令人满意。但是,原始大坝的上游路堤肩部在1937年7月施工结束前经历了一次深层的破坏,这是在紧邻Abberton的Chingford水库发生类似和众所周知的破坏的9天之前。尽管卡尔·特扎吉(Karl Terzaghi)的参与使Chingford的失败成为了土壤力学历史上的重要案例,并且标志着现代土壤力学原理的最早应用之一,但Abberton的失败仍是未知数,直到最近,当现有的失败者提出时大坝开始被考虑。本文介绍了先进的有限元分析方法,旨在分析阿伯顿原水坝的破坏和现有主水坝的稳定性。本构模型中使用的参数是根据可用的现场调查和实验室测试以及对伦敦粘土中其他破坏的反分析经验得出的。分析表明,原始路堤的上游肩部通过渐进破坏机制而破坏,该机制涉及坚硬的塑料伦敦粘土的顶部,而不是基础上的上冲积层。通过使用现代的土方设备,路堤的相对较快的填充速度对最初的大坝破坏做出了重要贡献。分析还显示了现有大坝在重建期间,第一次蓄水和长期内的令人满意的行为,其响应与观察到的相似。因此,针对阿伯顿原水坝和现有主水坝的观测行为,成功地对所使用的本构模型和导出的参数进行了校准,并可用于预测其拟建水坝期间和之后的水坝行为。

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