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Quantitative World Stress Map With Three Case Studies: Geologic Repository, Gold Mining and Deep Geothermal Energy

机译:具有三个案例研究的定量世界应力图:地质库,金矿和深层地热能

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Mechanical stress remains an enigmatic physical rock property due to the facts that stress cannot bernmeasured directly, it is difficult to visualize and it is affected by stress state-scale relations. Despite this,rnin situ rock stress has become a key parameter in rock engineering and solid Earth sciences, in general.rnIn this contribution, we focus on the state-of-the-art techniques determining the in situ stress at a givenrnsite by using our recently proposed rock stress terminology and applying the best-estimated stressrnmodel approach. In this context, we inform the reader on the existing World Stress Map databasern(WSM) of stress orientations, and our new database on lithologic in situ stress magnitudes, rockrnstrength and fracture mechanical properties, the so-called Quantitative WSM (Q-WSM). Three casernstudies highlight the road to the final rock stress model, which sometimes differs significantly from thernrecipes discussed. We address problems in obtaining reliable stress magnitudes in near-surface (0.5 km)rnhard rock of a Swedish radioactive waste disposal site, we report on stress perturbation due to minernexcavation close to a vertical dyke structure in a deep (3.5 km) South African gold mine, and werninvestigate Kaiser stress observations in a crystalline geothermal reservoir at 5 km depth applyingrnhydro-mechanical coupled discrete element modeling.
机译:由于不能直接测量应力,难以可视化并且受应力状态-比例关系的影响,机械应力仍然是一种神秘的物理岩石属性。尽管如此,一般而言,原位岩石应力已成为岩石工程和固体地球科学中的关键参数。在这一贡献中,我们专注于通过使用我们的技术来确定给定地点的原位应力的最新技术最近提出了岩石应力术语,并采用了最佳估计的应力模型方法。在这种情况下,我们向读者介绍现有的应力方向世界应力图数据库rn(WSM),以及有关岩性原位应力大小,岩壁强度和断裂力学性能的新数据库,即所谓的定量WSM(Q-WSM) 。三个案例研究突显了最终岩石应力模型的道路,有时与讨论的理论有很大不同。我们解决了在瑞典放射性废物处置场的近地表(0.5 km)坚硬岩石中获得可靠应力幅值的问题,我们报告了在深(3.5 km)南非金矿中接近垂直堤坝结构的矿床开挖引起的应力扰动矿井,并应用水力-机械耦合离散元模型研究了5 km深度的晶体地热储层中的Kaiser应力观测结果。

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