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Assessment of frictional resistance of granite rock joints with reference to weathering

机译:评估花岗岩岩接头的摩擦阻力参考风化

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Shearing resistance of rock joints is considered as one of the key aspects of rock masses as it is related to the stability of rock mass particularly at shallow surface condition. The shear behaviour of rock joints depends upon a number of influencing parameters and weathering state of discontinuity surface is one of them. However, over the years of research, the said issue has not been explored much. Hence this research presents primary findings aimed to explore the shearing resistance of unfilled rock joints regarding granites of different weathering grades. Multistage CNL direct shear tests were performed on six natural granite rock joints of two different but adjacent weathering grades at three different normal stress conditions ranging between 0.21 MPa - 0.7 MPa. It should be noted that the weathering grade of discontinuity surface was categorized following the six-fold weathering grade classification scheme, which was also substantiated with Schimdt rebound values. The data obtained from shear test was analysed in terms of stress ratio and peak friction angle, which shows the adverse effect of weathering with increasing normal stress condition. However, at low normal stress condition, such consequences were not significant.
机译:岩石接缝剪切性能被认为是的岩体的关键方面之一,因为它是特别是在浅表面状况相关的岩体的稳定性。岩石接头的剪切行为取决于许多影响参数和风化不连续面的状态的是其中之一。然而,在多年的研究,上述问题尚未探索多。因此,该研究提出的主要成果旨在探索空缺岩石节理就不同档次的风化花岗岩的的剪切性能。 0.7兆帕 - 多级CNL直剪试验是在三个不同的正常胁迫条件0.21兆帕之间的范围内的两个不同但相邻的风化等级六个天然花岗岩关节进行。应当指出的是,不连续面的耐候级被分类后的六倍耐候级分类方案,这也是与证实反弹Schimdt值。从剪切试验中获得的数据中的应力比和峰值摩擦角,其示出了具有增加正常应力条件风化的不利影响方面进行了分析。然而,在低正常胁迫条件下,这样的后果并不显著。

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