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首页> 外文期刊>Tunnelling and underground space technology >The application of distinct lattice spring model to zonal disintegration within deep rock masses
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The application of distinct lattice spring model to zonal disintegration within deep rock masses

机译:独特格点弹簧模型在深部岩体分区破裂中的应用

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摘要

Zonal disintegration has been frequently encountered in many tunnelling projects such as deep mining and water tunnels in hydropower stations. The mechanisms of this phenomenon cannot be explained reasonably through conventional mesh-based numerical approaches. Thus, in this study, a dual coupled Micro-Macro Continuum-Discontinuum approach named as Distinct Lattice Spring Model (DLSM) has been applied to investigate the mechanisms of zonal disintegration within deep rock masses. Firstly, the 3D numerical modes are built up, with fixed boundaries being set for far fields and displacement loading being applied along the tunnel axis. This numerical mode is then validated through comparing model simulation with laboratory model tests, where reasonable agreement has been achieved for all cases considered (normal rock mass and layered rock mass with different joint spaces). To cater for real tunnels within various rock masses, tunnels excavated in deep rock masses with different sizes, shapes and material heterogeneities are investigated. Numerical study demonstrates that, the DLSM is capable to reproduce the process of zonal disintegration explicitly, along with which the mechanical responses have been captured reasonably. It shows that, the occurrence of zonal disintegration mainly depends on the material heterogeneities and the in-suite stress level. The fracture patterns formed during zonal disintegration rely on tunnels' shape, size and the distribution of local weakness in surrounding rock masses.
机译:在许多隧道工程中,例如在水力发电站的深部采矿和水隧道中,都经常遇到区域分解的问题。无法通过常规的基于网格的数值方法合理地解释这种现象的机理。因此,在这项研究中,被称为离散晶格弹簧模型(DLSM)的双耦合微宏连续谱-不连续谱方法已被用于研究深部岩体中区域崩解的机理。首先,建立3D数值模式,为远场设置固定边界,并沿隧道轴施加位移荷载。然后,通过将模型模拟与实验室模型测试进行比较来验证这种数值模式,其中在所有考虑的情况下(正常岩体和具有不同节理空间的层状岩体)均已取得合理的共识。为了适应各种岩体中的真实隧道,研究了在深部岩体中开挖的具有不同尺寸,形状和材料异质性的隧道。数值研究表明,DLSM能够清晰地再现区域崩解的过程,并合理地捕获了机械响应。结果表明,区域崩解的发生主要取决于物质的非均质性和室内应力水平。层状崩解过程中形成的裂缝形态取决于隧道的形状,大小和围岩中局部弱点的分布。

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