肖尊群, 王鑫, 汤东桑, 董琼英, 姜亦男, 杨凯, 曹童童, 邓震. 巴东组典型红层软岩单轴压缩试验细观组构特征[J]. 煤田地质与勘探, 2019, 47(6): 103-114. DOI: 10.3969/j.issn.1001-1986.2019.06.017
引用本文: 肖尊群, 王鑫, 汤东桑, 董琼英, 姜亦男, 杨凯, 曹童童, 邓震. 巴东组典型红层软岩单轴压缩试验细观组构特征[J]. 煤田地质与勘探, 2019, 47(6): 103-114. DOI: 10.3969/j.issn.1001-1986.2019.06.017
XIAO Zunqun, WANG Xin, TANG Dongsang, DONG Qiongying, JIANG Yinan, YANG Kai, CAO Tongtong, DENG Zhen. Microscopic fabric characteristics of typical red soft rock in Badong Formation under uniaxial compression test[J]. COAL GEOLOGY & EXPLORATION, 2019, 47(6): 103-114. DOI: 10.3969/j.issn.1001-1986.2019.06.017
Citation: XIAO Zunqun, WANG Xin, TANG Dongsang, DONG Qiongying, JIANG Yinan, YANG Kai, CAO Tongtong, DENG Zhen. Microscopic fabric characteristics of typical red soft rock in Badong Formation under uniaxial compression test[J]. COAL GEOLOGY & EXPLORATION, 2019, 47(6): 103-114. DOI: 10.3969/j.issn.1001-1986.2019.06.017

巴东组典型红层软岩单轴压缩试验细观组构特征

Microscopic fabric characteristics of typical red soft rock in Badong Formation under uniaxial compression test

  • 摘要: 红色粉砂质泥岩和泥质粉砂岩是巴东组特殊性岩土的代表,具有遇水易崩解特性。根据岩样单轴压缩试验,基于PFC2D程序,建立中硬岩、软岩单轴压缩试验数值模型;模型选用平行黏结颗粒接触模型。根据应力-应变曲线特征,采用分段定量参数标定法对软岩试样的细观参数进行标定;且通过调整法向和切向黏结强度比值σc/τc,控制试样单轴压缩破坏模式;分别对不同风化程度的粉砂质泥岩和泥质粉砂岩在饱和、天然状态下单轴压缩试验过程进行模拟;并分析了试验过程中颗粒法向接触力、切向接触力、配位数、孔隙度等细观组构参数的分布特征和演化规律。研究结果表明:该数值方法能够很好地模拟中硬岩、软岩的单轴压缩试验过程,除中风化粉砂质泥岩外,风化程度和浸水条件仅能影响试样颗粒接触力在统计角度范围的大小,不能影响其分布形式;同时,风化程度和浸水条件延长了配位数显著下降的加载时间,配位数随裂缝数量的增加而减小;浸水条件和风化程度对泥质粉砂岩的孔隙度演化影响较大;风化程度对粉砂质泥岩孔隙度演化影响较大,而浸水条件影响较小。

     

    Abstract: Red silty mudstone and argillaceous siltstone are the representatives of special rock and soil in Badong Formation, are easy to disintegrate when encountering water. According to the uniaxial compression test of rock samples, a numerical model of medium and soft rock uniaxial compression test was established based on PFC2D program. With the characteristics of stress-strain curve, subsection quantitative parameter calibration method was used to calibrate the microscopic parameters of soft rock samples. The adjustment method and the ratio of tangential bond strength(σc/τc) control specimen under uniaxial compression failure mode. The uniaxial compression test of silty mudstone and argillaceous siltstone with different weathering degree under saturated and natural state was simulated. The distribution and evolution of meso-fabric parameters such as normal contact force, tangential contact force, coordination number and porosity were analyzed. The results show that the numerical method can well simulate the uniaxial compression test process of medium hard rock and soft rock. Except for medium weathered silty mudstone, weathering degree and water immersion condition can only affect the size of the contact force of sample particles in the statistical angle range, but cannot affect the distribution form. At the same time, weathering degree and water immersion condition prolonged the loading time of significantly decreased coordination number, which decreased with the increase of the number of cracks. Flooding condition and weathering degree have great influence on the porosity evolution of argillaceous siltstone. The degree of weathering has a great influence on the porosity evolution of silty mudstone, but the condition of flooding has little influence.

     

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