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Determining Young's Modulus of Fractured Coal Rock Mass through a Homogenization Method

机译:通过均质化方法确定缺口煤岩体的模量

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Three main fractures exist in coal rock mass, including face cleats, butt cleats, and major fractures. The distribution of cleats and beddings in coal rock mass likes a regular reticular. A geological model was established without considering the major fractures. Young's moduli of fractured coal rock mass were gained through a homogenization method monolayer composite micromechanics analysis method. The relations between volume fraction or Young's moduli of cleat and Young's moduli of coal rock mass were investigated by calculation. Results shown that Young's moduli of coal rock mass have the same change trends with the increase of volume fraction of cleat in the interval of 0.001-8mm of width of cleat. And the width of cleat of 0.5mm is a critical point. Young's moduli of coal rock mass monotonically increase with the increase of Young's modulus of cleat in the interval of 0.001-0.008GPa. Volume fraction and Young's moduli of cleats have notable effects on Young's moduli of coal rock mass.
机译:煤岩体存在三个主要骨折,包括面部夹板,对接夹板和主要骨折。煤炭岩体中的夹板和床上用品的分布喜欢常规网状。建立了地质模型,而不考虑主要骨折。通过均化方法单层复合微机械分析方法获得杨氏裂缝煤岩体的模态。计算通过计算研究了体积分数或杨氏模胶模型的关系。结果表明,杨氏煤岩体的模量具有相同的变化趋势随着夹层宽度0.001-8毫米的间隔而增加。并且纤维的宽度为0.5mm是临界点。年轻的煤岩体的Moduli在0.001-0.008GPa的间隔中随着杨氏模量的增加而单调地增加。体积分数和杨氏的微粒的Moduli对年轻的煤岩体的Moduli具有显着的影响。

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