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Evaluation on the Minimum Principal Stress State and Potential Hydraulic Jacking from the Shotcrete-Lined Pressure Tunnel: A Case from Nepal

机译:喷枪衬里压力隧道最小主应力状态和潜在液压升降的评价 - 来自尼泊尔的情况

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Reliable estimation of in situ stress state is very important in implementing unlined/shotcrete-lined pressure tunnels and shafts. The topography, local tectonic setting and geological environment greatly influence the magnitude of in situ stress level. This paper aims to evaluate in situ stress state at the Upper Tamakoshi Hydroelectric Project (UTHP), where unlined/shotcrete-lined headrace tunnel with considerable hydrostatic head is being implemented. Initially measured minimum principal stress indicated much lower values than the hydrostatic pressure at the downstream end of the headrace tunnel, which led to shift the alignment at the upper elevation with reduced hydrostatic pressure. In order to explore the reason behind much lower stress level as expected, a comprehensive assessment is carried out by developing a full rock stress model so that the minimum principal stress along the unlined pressure tunnel is evaluated. To address the complex geotectonic and topographic environment of the UTHP project area, a final rock stress model (FRSM) concept as suggested by Stephansson and Zang (2012) has been utilized. The FRSM concept considers stepwise evaluation of the in situ stress state analysis integrating the best estimate stress model (BESM), stress measurement methods (SMM) and integrated stress determination methods (ISD). The analysis carried out revealed that the in situ stress state at the project area has high degree of spatial variation even at the similar overburden due to the presence of complex topography and the presence of local shear and weakness zones. The analysis further demonstrates that a presence of local shear/weakness zone has considerable de-stressing effect, which leads to the reduction of in situ minimum principal stress magnitude. The reduction in the minimum principal stress along the pressure tunnel increases the risk for the potential hydraulic jacking and leakage if static water pressure is higher than the magnitude of minimum principal stress.
机译:在实现无衬里/喷射桥衬里的压力隧道和轴方面,对原位应力状态的可靠估计非常重要。地形,局部构造环境和地质环境极大地影响了原位应力水平的大小。本文旨在在上部Tamakoshi水力发电项目(UTHP)的原位应力状态下评估,其中,正在实施具有相当大的静水压头的无线/抽吸衬砌头部隧道。最初测量的最小主应力表明比头部隧道的下游端处的静液压压力大得多,这导致在上升升高处的对准,降低静压压力。为了探讨如预期的压力水平低得多的原因,通过开发完整的岩石应力模型进行综合评估,以便评估沿着无衬里压力隧道的最小主应力。为了解决UTP项目区域的复杂地理位置和地形环境,已经利用了Stephansson和Zang(2012)所建议的最终岩石压力模型(FRSM)概念。 FRSM概念考虑逐步评估原位应力状态分析,整合最佳估计应力模型(BESM),应力测量方法(SMM)和集成应力测定方法(ISD)。进行的分析表明,即使存在复杂地形的存在和局部剪切和弱点区域的存在,,项目区域的原位应力状态也具有高度的空间变化。该分析进一步证明了局部剪切/弱点的存在具有相当大的脱胁迫效果,这导致原位最小主应力幅度的降低。如果静电水压高于最小主应力的幅度,则沿压力隧道的最小主应力的降低增加了潜在的液压起重机和泄漏的风险。

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