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Effects of freezethaw on the determination and application of parameters of slope rock mass in cold regions

机译:冻融对寒冷地区边坡岩体参数确定与应用的影响

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摘要

Freeze-thaw could significantly affect the deterioration of mechanical properties of slope rock mass, and should be taken into consideration when determining the parameters of slope rock mass in cold regions. In this paper, we first measured the freeze-thaw coefficient using the freeze-thaw cycle test on intact slope rock mass from Mengku Mine, then determined the freeze-thaw correction coefficient by taking field geological investigation and rock hardness into consideration, and established a linear relationship between Geological Strength Index (GSI) and Tianshan slope rock mass rating (TSMR) system (a rock mass classification method applicable in cold regions) by incorporating the freeze-thaw correction coefficient into the expression of rock mass effect. The results show that freeze-thaw correction coefficient varies between 0.71 and 0.93, and GSI varies between 45 and 63. We further determined the parameters of slope rock mass by employing the generalized Hoek-Brown criterion and using it established a numerical rock slope excavation model and analyzed the rock mechanic features and stability status. The results indicate that the maximum ground deformation of slop rock mass is 15 mm, and the floor rebound is about 42 mm. Overall, the method described in the present paper can be used to select slope rock mass in cold regions and calculate the slope rock stability.
机译:冻融可显着影响边坡岩体力学性能的下降,在确定寒冷地区边坡岩体的参数时应予以考虑。本文首先对孟库矿完整边坡岩体进行冻融循环试验,测定冻融系数,然后结合野外地质调查和岩石硬度确定冻融校正系数,建立了冻融校正系数。通过将冻融校正系数纳入岩体效应的表达,将地质强度指数(GSI)与天山斜坡岩体额定值(TSMR)系统(一种适用于寒冷地区的岩体分类方法)之间的线性关系。结果表明,冻融校正系数在0.71至0.93之间变化,GSI在45至63之间变化。我们采用广义Hoek-Brown准则进一步确定了边坡岩体的参数,并使用它建立了数值岩石边坡开挖模型。并分析了岩石力学特征和稳定性状态。结果表明,边坡岩体的最大地面变形为15 mm,底板回弹约为42 mm。总体而言,本文所述方法可用于选择寒冷地区的边坡岩体并计算边坡岩体的稳定性。

著录项

  • 来源
    《Cold regions science and technology》 |2015年第2期|32-37|共6页
  • 作者单位

    Engineering Research Center of Rock-Soil & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan 430074, China Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;

    Engineering Research Center of Rock-Soil & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan 430074, China Faculty of Engineering, China University of Geosciences, Wuhan 430074, China,No. 388, Lumo Road, Wuhan 430074, Hubei, China;

    Engineering Research Center of Rock-Soil & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan 430074, China Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;

    Engineering Research Center of Rock-Soil & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan 430074, China Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;

    Engineering Research Center of Rock-Soil & Excavation and Protection of Ministry of Education, China University of Geosciences, Wuhan 430074, China Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Cold region; Slope rock mass; Freeze-thaw coefficient; Freeze-thaw correction coefficient; Generalized Hoek-Brown criterion;

    机译:寒冷地区;斜坡岩体;冻融系数;冻融校正系数;广义Hoek-Brown准则;

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