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

机译:现场弱岩带变形模量的预测研究

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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:弱岩带(软夹层,断层带和软岩)是大规模地质工程研究的重点。这是分析岩体稳定性的重要边界。长期的地质时期形成了较弱的岩石带,在此期间,各种岩石经历了地应力和构造应力的长期固结。因此,在原位条件下,它们的密度和变形模量相对较高。由于其碎片性,一旦暴露于地球表面,弱岩石区的结构将很快松散,密度将降低,变形模量也将大大降低。通常,在大型建设项目中,尤其是在水电站的坝基岩中,会发现薄弱的岩层。这些岩石不能通过挖掘完全消除。此外,现今的所有测试都是在弱岩带暴露之后进行的,无法揭示原位条件下的变形模量。在这篇论文中,我们的研究人员提出了一种测试方法。该方法是整体多层介质变形方法。不必消除覆盖在较弱岩石区域上的相对完整的岩石。还介绍了用于在各种介质中获得变形模量的理论公式。在等效密度条件下进行了现场比较试验和室内变形模量试验。我们采用了几种方法对原位条件下的弱岩带变形模量进行预测研究,并揭示了一个事实,即在原位条件下,弱岩带的变形模量比经过试验获得的测试结果高出好几倍。曝光。从地质工程的角度来看,研究成果从根本上改变了人们对弱岩带变形模量的观念,为精确定义盖岩条件下深层弱岩带的变形模量提供了重要的理论和方法,如以及合理的工程应用。

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