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Prediction research of deformation modulus of weak rock zone under in-situ conditions

机译:原位条件下弱岩区变形模量预测研究

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Weak rock zone (soft interlayer, fault zone and soft rock) is the highlight of large-scale geological engineering research. It is an important boundary for analysis of rock mass stability. Weak rock zone has been formed in a long geological period, and in this period, various rocks have undergone long-term consolidation of geostatic stress and tectonic stress; therefore, under in-situ conditions, their density and modulus of deformation are relatively high. Due to its fragmentary nature, once being exposed to the earth's surface, structure of weak rock zone will soon be loosened, its density will be reduced, and its modulus of deformation will also be reduced significantly. Generally, weak rock zone can be found in large construction projects, especially in the dam foundation rocks of hydropower stations. These rocks can not be eliminated completely by excavation. Furthermore, all tests nowadays are carried out after the exposure of weak rock zone, modulus of deformation under in-situ conditions can not be revealed. In this thesis, a test method ex- plored by our researchers has been introduced. This method is a whole multilayered medium deformation method. It is unnecessary to eliminate the relatively complete rocks covering on weak rock zone. A theoreti- cal formula to obtain the modulus of deformation in various mediums has also been introduced. On-site comparative trials and indoor deformation modulus tests under equivalent density conditions have been carfled out. We adopted several methods for the prediction researches of the deformation modulus of weak rock zone under in-situ conditions, and revealed a fact that under in-situ conditions, the deformation modulus of weak rock zone are several times higher than the test results obtained after the exposure. In a perspective of geological engineering, the research findings have fundamentally changed peoples' concepts on the deforma- tion modulus of weak rock zone, provided important theories and methods for the precise definition of deformation modulus of deep weak rock zone under cap rock conditions, as well as for reasonable engineering applications.
机译:弱岩区(软层间,断层区和软岩)是大规模地质工程研究的亮点。它是分析岩体稳定性的重要边界。弱岩区已形成在较长的地质时期,并且在此期间,各种岩石经历了长期整理的地静压和构造应力;因此,在原位条件下,它们的密度和变形模量相对较高。由于其局部性质,一旦暴露在地球表面,弱岩区的结构将很快松开,其密度将减小,其变形模量也将显着降低。一般来说,弱岩区可以在大型建筑项目中找到,特别是在水电站的大坝基础岩石中。这些岩石不能完全通过挖掘来消除。此外,现在进行所有测试在弱岩区域暴露后进行,不能揭示原位条件下的变形模量。本文介绍了我们研究人员进行的测试方法。该方法是全多层介质变形方法。不需要消除覆盖弱岩区的相对完整的岩石。还介绍了在各种介质中获得变形模量的理论。在现场比较试验和室内变形模量试验在等效密度条件下被耗尽。我们采用了几种方法对原位条件下弱岩区变形模量的预测研究,并揭示了在原位条件下,弱岩区的变形模量比在原位状况下比获得的测试结果高出几倍曝光。在地质工程的角度下,研究结果从根本上改变了人们对弱岩区的变形模量的概念,为帽岩条件下深弱岩区变形模量的精确定义提供了重要的理论和方法。以及合理的工程应用。

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