覆岩采动裂隙演化形态的相似材料模拟实验  

Model experiment of evolution pattern of mining-induced fissure in overlying strata

作　　者：林海飞[1,2] 李树刚[1,2] 成连华[1,2] 王红胜[1,2] 

机构地区：[1]西安科技大学能源学院,陕西西安710054 [2]教育部西部矿井开采及灾害防治重点实验室,陕西西安710054

出　　处：《西安科技大学学报》2010年第5期507-512,共6页Journal of Xi’an University of Science and Technology

基　　金：国家自然科学基金项目(50874098);高等学校博士学科点专项科研基金(20096121110002);西安科技大学博士启动基金(A5030117);西安科技大学培育基金(2009008)

摘　　要：煤层开采后,覆岩采动裂隙演化规律及其形态特征与卸压瓦斯抽采密切相关。通过沿工作面走向及倾向相似材料模拟实验,得到覆岩采动破断裂隙的产生、发展为三阶段演化规律,形态呈"M"状。离层裂隙呈两大阶段、两个层位、三个区间的演化特征,即在主关键层触矸前,分布形态在垮落的最上位亚关键层上部,呈倒"V"状,下部呈"M"状;当主关键层触矸后,主关键层下部离层分布形态呈"M"状,上部少有离层发育。基于此,得到了覆岩采动裂隙演化形态与特征,提出了"采动裂隙圆角矩形梯台带"工程简化模型,为确定卸压瓦斯抽采钻孔参数提供了一定理论依据。After mining,the evolution law and distribution features of mining fissure in overlying strata are closely related to the degasification of relieved methane.Using the model experiment along strike and dipping direction of face,it is obtained that the generation and development of mining broken fissure has three stage evolution laws,and its pattern is ＂M＂.The bed-separated fissure has two stages,two horizons and three regions evolution features.Before the main key stratum touch the gangue,the pattern of bed-separated fissure is inverse ＂V＂ above the upper falling sub-key stratum,and is ＂M＂ below the upper falling sub-key stratum.After the main key stratum touched the gangue,the pattern of bed-separated fissure is ＂M＂ below it,and bed-separated fissure develops few above it.Based on these,the evolution patterns and features of mining-induced fissure are obtained,the engineering simplified model of mining-induced fissure round-rectangle trapezoidal zone is put forward.It provides the foundation for conveniently and reasonably determining the parameters of degasfication drill hole of relieved methane.

关 键 词：采动裂隙 演化形态 圆角矩形梯台带 相似材料实验 

分 类 号：TD713[矿业工程—矿井通风与安全]