基于FLAC采场底板应力-应变本构关系研究
Study on stress-strain constitutive relation of coal bed floor based on FLAC
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摘要: 矿山压力是影响底板承压水突出的重要因素,是底板破坏的力源;了解煤层底板的应力分布是研究煤层底板破坏深度的重要前提,有利于加深对突水机理的认识。本文采用FLAC模拟软件求解采场的围岩应力-应变关系,分析了不同阶段采空区底板应力变化过程,并根据底板不同深度的垂直应力与垂直位移值,运用数学方法建立应力、应变随采场深度变化的本构方程。结果表明:随着深度的增加,垂直应力逐步增加,底板垂直应力σy为底板深度X的二次函数,而垂向位移逐步减小,底板垂直方向的应变ε为底板深度X的负指数函数。Abstract: As the force source of floor destruction,ground pressure is the main factor for the problem of confined water inrush.For studying coal floor damage depth and acquiring more knowledge of water-inrush mechanism,it's an important precondition to know the pressure distribution in the coal seam floor.The stope surrounding rock stress-strain relationship and goaf floor stress distribution in different stage has been analyzed by the simulation of FLAC.According to the vertical stress and strain in the floor of different depth,mathematical method was used to get stress-strain constitutive equations changing with stope depth.The result shows that with the increase of depth,the vertical stress is gradually increased,but vertical displacement reduced gradually.The floor vertical stress σy is a quadratic function of the floor depth X.The floor strainε in vertical is a negative exponential function of the floor depth X.
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