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Assessment on stress induced instability in a tunnel project of the Himalaya

机译:喜马拉雅山隧道工程中应力诱发失稳的评估

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In the Himalaya, the majority of long tunnels face severe tunnel instability problems. One of the major instability is related to rock stresses. The headrace tunnel of Parbati II hydroelectric project is one of the long tunnel systems that is facing severe stress induced instability. Especially this has been the case in the tunnel segment passing through Manikaran quartzite. It is known fact that the extent and type of stress induced instability vary greatly upon the rock type, deformability properties of the rock in question, and jointing and inter-bedding characteristics in the rock mass. This paper reviews most important rock mechanical properties that may have direct link on the nature of stress induced instability. It also back calculates magnitude of in-situ stress state in the project. An attempt is made to establish tectonic component of the horizontal stress. It is hoped that calculated stress magnitude may be useful for further stability assessment.
机译:在喜马拉雅山,大多数长隧道面临着严重的隧道失稳问题。主要的不稳定性之一与岩石应力有关。 Parbati II水电站的引水隧洞是长隧道系统之一,面临着严重的应力诱发的不稳定性。特别是在穿过Manikaran石英岩的隧道段中就是这种情况。众所周知的事实是,应力引起的不稳定性的程度和类型随岩石的类型,所讨论岩石的可变形性以及岩体中的节理和层间特性而有很大差异。本文回顾了最重要的岩石力学性质,这些性质可能与应力诱发的不稳定性具有直接的联系。它还可以反算项目中的原地应力状态的大小。试图建立水平应力的构造分量。希望计算出的应力大小可能有助于进一步的稳定性评估。

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