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Identification of the Hydro-Mechanical in- Situ Properties of Tournemire Argillite from Mine-by-test Experiment

机译:鉴定逐次试验实验的塔内夏骨质野石的水力机械原位特性

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A mine-by-test was performed in the IRSN experimental site in the Tournemire argillite, during the excavation of a new gallery in 2003. Thanks to the various measurements of pore pressure and displacements then recorded, it has been possible to identify by inverse analysis the in situ hydro-mechanical properties of the rock mass. The use of the convergence-confinement method enables us to reproduce the main tendencies of most of the recorded measurements. In addition, viscoplastic calculations have been performed in order to appraise the origin of the delayed response of the rock mass.
机译:在2003年开挖新廊的挖掘过程中,在赛车古尔岛的IRSN实验部位进行了一种逐次测试。由于记录了孔隙压力和位移的各种测量,因此可以通过逆分析识别岩体的原位水电性能。收敛限制方法的使用使我们能够再现大多数记录测量的主要趋势。此外,已经进行了粘性计算,以评估岩体延迟响应的起源。

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