魏宗勇;李树刚;林海飞;双海清;丁洋;

• 1:西安科技大学安全科学与工程学院
• 2:西安科技大学西部矿井开采及灾害防治教育部重点实验室

摘要(Abstract)：

上覆岩层裂隙区域是瓦斯运移储集通道,为准确得到大采高综采条件下裂隙演化特征,以山西天池煤矿202工作面为原型搭建了三维物理相似模拟模型,采用声发射监测系统、三维模型剖切等方法得到覆岩裂隙发育过程及裂隙分布特征。结果表明,202工作面基本顶初次垮落步距为36 m,周期来压步距为16～27 m,周期来压平均步距18 m;采用物理模型剖切的方式得到采动覆岩裂隙高度及三维分布形态,垮落带高度15 m,是采高2.9倍,裂隙带高度64 m,是采高12.5倍;覆岩垮落裂隙三维形态为"椭抛体"。在煤层倾向及走向上,覆岩整体下沉趋势为"凹"型,距离煤层底板10 m处上覆岩层下沉量最大为3.5 m,越往上下沉量越小,岩层下沉呈梯形分布;在走向及倾向方向裂隙密度均呈现"双驼峰"状,倾向裂隙区位于工作面0～30 m与90～120 m范围内,走向裂隙区位于切眼侧0～30 m与停采线侧160～200 m范围内,裂隙区裂隙密度达5条/m,中部压实区裂隙密度在1～2条/m之间,回风巷侧裂隙区为高位巷布置最佳区域,能够有效提高瓦斯抽采效率,对工作面及采空区瓦斯治理具有重要意义。

关键词(KeyWords)： 大采高;综采工作面;三维实验;声发射;模型剖切;裂隙演化

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金(51704228,51704227)

作者(Author): 魏宗勇;李树刚;林海飞;双海清;丁洋;

Email:

DOI: 10.13800/j.cnki.xakjdxxb.2020.0405

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