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迟世春, 王腾腾, 贾宇峰. 堆石料颗粒的延迟破碎时间研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20230074
引用本文: 迟世春, 王腾腾, 贾宇峰. 堆石料颗粒的延迟破碎时间研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20230074
Study on delayed breaking time of rockfill materials particles[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20230074
Citation: Study on delayed breaking time of rockfill materials particles[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20230074

堆石料颗粒的延迟破碎时间研究

Study on delayed breaking time of rockfill materials particles

  • 摘要: 堆石料颗粒的延迟破碎是指颗粒受力一定时间后发生的破碎。给出颗粒延迟破碎时间是采用离散元法模拟堆石料流变进行定量分析的前提。本文从断裂力学出发,将颗粒内部缺陷概化为一币形裂纹,给出了颗粒瞬时破碎强度与裂纹半长的关系。视颗粒瞬时强度为随机变量,采用Logistic函数描述其分布,并运用求解随机变量函数概率分布的方法,求出裂纹半长的概率分布。然后进行颗粒岩石的双扭松弛试验,测量其亚临界裂纹扩展速度参数。对颗粒裂纹扩展方程进行积分,得到裂纹贯通(即颗粒延迟破碎)的时间表达式。以裂纹半长为随机变量,可求出颗粒延迟破碎时间的概率分布。云南红石岩工程白云岩颗粒的相关计算表明,在相同应力水平下,大颗粒延迟破碎时间长且离散性大,小颗粒延迟破碎时间短且离散性小。这与堆石料室内流变试验稳定快而现场堆石坝流变持续时间长的宏观现象相吻合。颗粒延迟破碎时间的给出为采用离散元模拟堆石料流变,提升堆石料流变本构模型,解决堆石料流变室内试验的时间尺寸效应奠定了基础。

     

    Abstract: The delayed crushing of rockfill particles is specifically referring to the crushing of particles after loading for a certain time. It is a prerequisite for quantitative analysis of rockfill rheology by using discrete element method to give the particle delay breaking time. In this paper, from the point of view of fracture mechanics, the internal defects of particles are generalized into a one-dollar crack, and the relationship between the instantaneous crushing strength of particles and the half-length of the crack is given. Logistic function was used to describe the distribution of particle strength as random variable, and the probability distribution of crack half-length was obtained by using the method of solving the probability distribution of random variable function. The bi-torsional relaxation test of granular rock was carried out to measure the sub-critical crack propagation velocity parameter, and the time expression of crack penetration (i.e., particle delayed crushing) was obtained by integrating. The probability distribution function of particle delay breaking time can be obtained by taking the crack half-length as random variable. The calculation results of dolomite particles in redstone project in Yunnan province show that, under the same stress conditions, large particles have long delay time and large standard deviation, while small particles have short delay time and small standard deviation. This is consistent with the macro phenomenon that rheological deformation of rockfill materials converges quickly in laboratory test, while rheological deformation of rockfill dam lasts a long time in field. The calculation results of particle delay breaking time provides basic conditions for using discrete element to simulate rockfill rheology, improving the rockfill rheological constitutive model, and solving the time-size effect of rockfill rheology for laboratory test.

     

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