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A study on the uplift mechanism of Tongjiezi dam using a coupled hydro-mechanical model

机译:铜界子大坝升力机理的水力耦合模型研究。

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During filling in 1992 of the Tongjiezi reservoir, in Southwest China, it was noticed that the dam body and the rock masses on the right side of the valley were uplifted up to 22.2 mm and 24.3 mm respectively. After reservoir filling in 1993, the uplift continued, but the rate decreased, and the measured maximum uplift increased from 22.2 mm to 27.5 mm in the dam body and from 24.3 mm to 28.9 mm in the rock masses from 1993 to 2004. Based on the geological features of the dam site and observed geomechanics data, a numerical method is used to evaluate the representative elementary volume (REV) and to identify the parameters related to the mechanical and hydraulic properties of the rock mass. Furthermore, a coupled hydromechanical model is presented to describe the uplift process. The simulated results agree well with those measured. In addition, the time-dependent deformation is studied in the laboratory and numerically. It is concluded that, with the specific hydrogeological conditions at the Tongjiezi dam site, hydro-mechanical coupling during and after the reservoir impoundment is the main factor contributing to the uplift, and the time-dependent deformation is due to the rheological behavior of rock masses under seepage pressure.
机译:在中国西南地区的通jie子水库于1992年充填水时,注意到坝体和山谷右侧的岩体分别被抬升至22.2 mm和24.3 mm。在1993年水库充填后,隆起继续,但速率减小,从1993年至2004年,测得的坝体最大隆起从22.2 mm增加到27.5 mm,岩体中最大隆起从24.3 mm增加到28.9 mm。坝址的地质特征和观测到的地质力学数据,采用一种数值方法来评估代表性基本体积(REV)并确定与岩体的机械和水力特性有关的参数。此外,提出了耦合流体力学模型来描述隆升过程。仿真结果与实测结果吻合良好。另外,在实验室和数值上研究了随时间变化的变形。结论:在同节子坝坝址特定的水文地质条件下,水库蓄水期间和之后的水力耦合是引起隆升的主要因素,且随时间变化的变形归因于岩体的流变行为。在渗透压力下。

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