纸质出版:2017
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[1]王林峰,唐红梅,陈洪凯,叶四桥,唐芬.温度-应力联合作用下的不稳定岩块稳定性分析[J].防灾减灾工程学报,2017,37(06):871-877.
王林峰, 唐红梅, 陈洪凯, et al. Temperature and Stress Combined Effect on the Unstable Rock Block Stability Analysis[J]. 2017, 37(6): 871-877.
[1]王林峰,唐红梅,陈洪凯,叶四桥,唐芬.温度-应力联合作用下的不稳定岩块稳定性分析[J].防灾减灾工程学报,2017,37(06):871-877. DOI: 10.13409/j.cnki.jdpme.2017.06.003.
王林峰, 唐红梅, 陈洪凯, et al. Temperature and Stress Combined Effect on the Unstable Rock Block Stability Analysis[J]. 2017, 37(6): 871-877. DOI: 10.13409/j.cnki.jdpme.2017.06.003.
在温差较大的区域
温度是诱发薄型不稳定岩块崩落的重要因素之一。考虑温度与应力联合作用下对不稳定岩块稳定性的影响
首先基于传热学方法
将x
y两个方向的温度传递分别进行计算
然后通过叠加原理建立了不稳定岩块内温度场和不稳定岩块主控结构面处的温度应力解析计算方法。考虑温度应力、不稳定岩块自重、地震和裂隙水压力联合作用下
基于断裂力学建立了不稳定岩块主控结构面的应力强度因子的计算方法
并根据不稳定岩块主控结构面的联合应力强度因子和断裂韧度构建了不稳定岩块稳定性分析方法。通过算例对比分析
结果表明
温度应力对薄型不稳定岩块的稳定性有着重要的影响
温度刚开始升高时不稳定岩块的稳定系数下降较快
随着温度进一步升高
不稳定岩块的稳定系数变化变缓;揭示了温度和主控结构结构面贯通长度联合作用下不稳定岩块稳定性的变化规律。所建立的不稳定岩块稳定系数计算方法可为温差较大地区的薄型不稳定岩块稳定性分析提供新的方法。
One of the important factors for collapse of thin and unstable rock block is temperature in the areas with large temperature difference. This paper will consider the effect of stability on unstable rock block under the combination of temperature and stress. Firstly
calculating the temperature transfer in x and y direction respectively on the basis of the heat transfer method
and then establishing the computing method of temperature stress in temperature field and master structure plane of unstable rock mass by using superposition principle. Considering the combination of temperature stress
the unstable rock mass weight
earthquake and fissure water pressure
we established the calculation method of stress intensity factor of the master structure plane of unstable rock mass based on fracture mechanics
and then according to combination stress intensity factor of the master structure plane of unstable rock mass and fracture toughness to construct the stability analysis method of unstable rock mass. The comparative analysis shows that temperature stress has a significant influence on stability of thin and unstable rock mass. At the beginning of temperature rising
the stability coefficient of unstable rock mass decreases quickly
and with the temperature rising further
the stability coefficient of unstable rock mass changes slowly
which reveals the stability variation law of unstable rock block under the combined action of temperature and the perforation’s length of master control structure plane. The stability coefficient compute method of unstable rock mass in this paper can provide new approach to stability analysis of thin and unstable rock block in large temperature difference areas.
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