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Influence of topography on in situ stress parameter at the proposed powerhouse sites of Rupaligad re-regulating project, Nepal

机译:地形对鲁佩加拉德重新调控项目的拟议促进工程的原位应力参数的影响

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In-situ stress parameters of the rock mass are one of the vital inputs for the design of any large underground openings. In general, the in-situ stress magnitude and orientation are influenced by topography, and major geological structures like folds, faults and intrusions. These structures bring about local heterogeneities in rocks, thus leading to change in orientation of stress trajectories. In this paper we would like to present a case study about the influence of topography/valley on in situ stress measurements carried out at a hydroelectric project site. The stress measurements were carried out by HTPF method on both left and right banks of the river at the proposed powerhouse sites. The test site/borehole location of left bank is in close proximity to valley compared to its counterpart. The (in-situ stress) major horizontal principal stress direction of the rock mass is N 20° and N 130° at right and left banks respectively. It is inferred that the horizontal stresses might have been relaxed due to the absence of influence of topography on the right bank whereas the direction of in-situ stress tensor at the left bank might be perturbed by topography due to the close proximity of the valley.
机译:岩体的原位应力参数是任何大地下开口设计的重要输入之一。通常,原位应力幅度和方向受到地形的影响,以及折叠,故障和入侵等主要地质结构。这些结构带来了岩石中的局部异质性,从而导致应力轨迹的取向变化。在本文中,我们想提出一个关于地形/谷对水电项目现场进行的原位应力测量影响的案例研究。通过HTPF方法在促成的促进州地点的河流左右银行上进行应力测量。与其对应物相比,左岸的测试站点/钻孔位置靠近谷。 (原位应力)岩体的主要水平主应力方向分别位于右侧和左岸的N 20°和N 130°。推断推断出由于右岸上的地形的影响而可能已经放松了水平应力,而由于谷的近距离接近,左侧的原位应力张力的方向可能被扰动。

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