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Coupled modeling of Excavation Damaged Zone in Boom clay: Strain localization in rock and distribution of contact pressure on the gallery's lining

机译:动臂粘土中开挖损伤区的耦合模型:岩石中的应变局部化和画廊衬砌上的接触压力分布

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Around galleries excavated at depth in geological media, the creation of a damaged zone with significant irreversible deformation is generally unavoidable. In the case of a geological disposal system for high-level radioactive waste, the resulting change in the host rock properties in this damaged zone may potentially be important with respect to the long-term evolution and the performance of that system. In this context, predicting the extent of the so-called Excavation Damaged Zone (EDZ) and, possibly, the fractures' network topology remains a challenge. This study is aimed to simulate numerically the extension of this zone at the large scale's excavation, around the Connecting gallery (HADES URL, Mol, Belgium), in Boom clay host rock through analyzing the evolution of strain localization in shear bands mode. To realistically model the involved phenomena, the concrete lining is considered on the gallery wall highlighting its impacts on the evolution of convergence and EDZ around the gallery. The focus of the current paper is made on analyzing the coupled hydro-mechanical behavior of Boom clay host rock during and after the gallery excavation with respect to the evolution of localized shear bands around the gallery. This study is accompanied by the analysis of the contact mechanism on the interface between the clay massive and the lining. The obtained results reveal some interesting features regarding the contact phenomenon relatively to the evolution pattern of shear bands within the clay around the gallery. To assess the reliability of the proposed approach, a discussion on some in-situ observations during the gallery's construction is also performed based on which a good agreement is found between the in-situ evidence and simulated results. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在地质介质深处开挖的廊道周围,不可避免地会产生不可逆变形的损坏区域。对于用于高放废物的地质处置系统,在该受损区域中,主岩属性的最终变化对于该系统的长期演化和性能而言可能是重要的。在这种情况下,预测所谓的“基坑破坏带”(EDZ)的范围以及可能的裂缝网络拓扑仍然是一个挑战。本研究旨在通过分析剪切带模式下应变局部化的演变,以数值模拟该区域在动臂粘土宿主岩中连接廊(HADES URL,摩尔,比利时)周围的大规模开挖扩展。为了真实地模拟所涉及的现象,在画廊的墙壁上考虑了混凝土衬里,以突出其对画廊周围的收敛性和EDZ演变的影响。本文的重点是分析廊道开挖期间和之后的动臂粘土基质岩石的耦合水力行为,以了解廊道周围局部剪切带的演化。这项研究伴随着对粘土块与衬砌之间界面接触机理的分析。获得的结果揭示了一些与接触现象有关的有趣特征,这些特征相对于画廊周围粘土内剪切带的演化模式而言。为了评估所提出方法的可靠性,还对画廊建设过程中的一些现场观察进行了讨论,并在此基础上找到了现场证据与模拟结果之间的良好协议。 (C)2015 Elsevier Ltd.保留所有权利。

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