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Engineering geological characterization and comparison of predicted and measured deformations of a cavern in the Italian Alps

机译:意大利阿尔卑斯山洞穴的工程地质特征以及预测和实测变形的比较

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摘要

A detailed engineering geological characterization and performance monitoring were carried out at the site of an underground powerhouse cavern in the Italian Alps. In the area of the hydroelectric project, consisting of a 4-m diameter and 10-km-long diversion tunnel and a powerhouse cavern (20 m wide, 39 m long and 30 m high), metamorphic anisotropic rocks, are present. A pervasive foliation, whose trend describes an open fold at the cavern site, characterizes the geological structure. The studies include petrographic analyses and geo-mechanical properties of the rocks, in situ stress measurements and rockmass classifications for the cavern site as well as the surrounding area. Based on field investigations, two numerical models (FEM and DEM codes) were used to investigate the overall stability of the excavation and to predict the expected deformation caused by each excavation phase. The measurements of actual deformations, by multi-base extensometer data, are reasonably close to those predicted through the numerical approaches.
机译:在意大利阿尔卑斯山的地下厂房洞穴中进行了详细的工程地质特征和性能监控。在该水电项目区域,存在一条直径为4 m,长10 km的引水隧洞和一座厂房洞室(宽20 m,长39 m,高30 m),是变质的各向异性岩石。普遍的叶面特征是地质结构的特征,其趋势描述了洞穴部位的开放褶皱。这些研究包括岩石的岩石学分析和地质力学特性,洞穴位置以及周围地区的现场应力测量和岩体分类。在现场调查的基础上,使用了两个数值模型(FEM和DEM代码)来研究开挖的整体稳定性,并预测每个开挖阶段引起的预期变形。通过多基引伸计数据对实际变形的测量与通过数值方法预测的结果相当接近。

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