煤层不同含水率对采场稳定性的影响

    Influence of Different Moisture Content of Coal Seams on Stope Stability

    • 摘要: 煤层在开采过程中,经常会受到水害的影响。由于水对煤体的物理化学作用,导致煤体弱化,从而影响到采场围岩应力的分布异于未受地下水威胁的采场。为了研究不同含水率对采场稳定性的影响,首先测定了煤体在不同含水率下(3%、6%、9%)的相关物理力学参数,然后通过理论分析和数值模拟软件分别对不同含水率下煤层沿走向推进一定距离后,煤层围岩体的稳定性进行分析研究。研究结果表明:在工作面推进了同样的距离后,随着煤层含水率的升高,煤柱应力集中系数减小,峰值应力向远离煤壁方向转移,采空区顶板破坏区域变大。同时,含水率的增加,对底板变形的影响不大。

       

      Abstract: In the process of mining, coal seam will be often affected by the flood. The physical and chemical interactions between water and coal result in the weakening of coal, which affects the stress distribution and stability of surrounding rock of face. In order to study the influence of moisture content on stress distribution at mining face, the physical and mechanical parameters under different water content (3%, 6%, 9%) in coal were firstly determined, and then theoretical analysis and numerical simulation were used to analyze the stability of coal seams in different moisture content while the face was promoted to a certain distance in the trend. The results show that: after the working face advanced the same distance, as moisture content of the coal seam increases, the coal pillar stress concentration coefficient will decrease, the peak stress will transfer to be far from the coal wall, and the damage area of the gob roof will grow larger. At the same time, the increase of water content has relative little effect on the floor deformation.

       

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