付帅, 栗婧, 解北京, 张明杰, 吕平洋, 牟林桐. 平顶山矿区突出能量分布规律及其控制因素[J]. 煤矿安全, 2016, 47(7): 182-185,189.
    引用本文: 付帅, 栗婧, 解北京, 张明杰, 吕平洋, 牟林桐. 平顶山矿区突出能量分布规律及其控制因素[J]. 煤矿安全, 2016, 47(7): 182-185,189.
    FU Shuai, LI Jing, XIE Beijing, ZHANG Mingjie, LYU Pingyang, MU Lintong. Outburst Energy Distribution and Its Controlling Factors in Pingdingshan Mining Area[J]. Safety in Coal Mines, 2016, 47(7): 182-185,189.
    Citation: FU Shuai, LI Jing, XIE Beijing, ZHANG Mingjie, LYU Pingyang, MU Lintong. Outburst Energy Distribution and Its Controlling Factors in Pingdingshan Mining Area[J]. Safety in Coal Mines, 2016, 47(7): 182-185,189.

    平顶山矿区突出能量分布规律及其控制因素

    Outburst Energy Distribution and Its Controlling Factors in Pingdingshan Mining Area

    • 摘要: 根据平顶山矿区内部分矿井实测三向应力、瓦斯含量、压力值计算了各矿区煤层弹性能及瓦斯膨胀能,并分析了其分布规律及特点,结合平煤矿区3次地质运动及矿区内地质构造特性,得到了突出潜能的主要控制因素并进行突出危险性划区。结果显示:弹性能及瓦斯膨胀能随埋深增加而增加,受地质构造控制作用显著;自重应力场控制区域煤层弹性与瓦斯膨胀能远小于构造应力场控制区域;构造应力控制区域随埋深增加构造控制作用逐渐减弱,转变为自重应力控制作用;自重控制区域煤层单位体积煤体瓦斯膨胀能与弹性近似相等,而构造应力控制区域膨胀能远大于弹性形;地质构造控制着矿区突出潜能的分布,是矿区突出主要控制因素;锅底山与九里山断层间区域危险性最小,锅底山与李口向斜之间突出危险性偏高,而李口向斜东南部区域突出危险性最高。通过对矿区突出点分布情况分析证明了突出危险性划区的正确性。

       

      Abstract: According to the in-situ three-dimensional stress, gas content and pressure value of some coal mines in Pingdingshan Mining Area, elastic energy and gas expansion energy were calculated. And combining with three main geological movements and structure distribution in Pingdingshan Mining Area, controlling factors of outburst energy were analyzed. The results show that elastic energy and gas expansion energy increase with the burial depth and are controlled by tectonic stress; elastic energy and gas expansion energy in self-weight stress field are much lower than that in tectonic stress field; tectonic control effect is gradually weakened with the burial depth and changing to self-weight stress field in regional tectonic stress field; gas expansion energy contained in unit volume of coal is approximately equal to elastic energy in self-weight stress field and is much higher than elastic energy in tectonic stress field; geological structures control the distribution of outburst energy and is the main controlling factor of outburst; zone between Guodishan fault and Jiulishan fault has the lowest risk of outburst, and zone between Guodishan fault and Likou syncline has a higher risk and zone in southeast of Likou syncline has the highest outburst risk. The analysis of outburst accidents in Pingdingshan Mining Area proves that the outburst risk division is right.

       

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