采场上覆岩层塑性断裂区域和移动规律研究
A study on the plastic fracture region and its movement in overlying rock bed in mining stope
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摘要: 采场岩体一面临空,上覆围岩的应力由原来的三向应力状态变为二向应力状态。在次生应力的作用下,随工作面的推进,上覆岩层将出现受拉区和塑性区。为此,提出了岩体断裂失稳的应力判据,该判据可以计算出顶板的拉应力区、塑性断裂区和O型圈的范围。并以白皎煤矿地质资料为背景,用3D-σ有限元分析软件,建立了采场的三维结构模型,用应力判据结合数值分析的结果,计算出了顶板拉应力区、塑性断裂区和O型圈的范围;并分析了不同步距老顶受拉区、塑性区、O型圈和顶板沉降的演化特征。研究成果可为采场压力计算和控制提供理论依据。Abstract: Due to the one-side suspending of rock mass in mining stope, the stress from overlying country rock changed from three-dimensional stress state into two-dimensional stress state. With the face advance under the working of secondary stress, in overlying rock mass will appear tensile region and plastic region. Therefore, the criterion of destabilization by rock creep fracture has been brought forward to figure out the tensile force region, plastic fracture region and . O-outlined circle range on roof. The experiment in this essay is based on the geologic informatics of the coal mine in Bai Jiao and to set up a 3-D Structural Model with 3D-σ finite-element software. By the application of stress criterion and numeric analysis, he tensile force region, plastic fracture region and . O-outlined range on the roof were defined out. The essay also analyzed the evolvement of tensile force region with different paces, plastic region, O-outlined circle and roof sedimentation. The results will provide theoretical proof for stress calculation and control of mining stope.
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