
Vol. 45 No. 3 Jun.2018
矿业安全与环保
MINING SAFETY & ENVIRONMENTAL PROTECTION
李守锋,届英.基于震源机制的煤矿采动主应力场反潢分析[J].矿业安全与环保,2018,45(3):90-93 文章编号:10084495(2018)03009004
第45卷第3期 2018年6月
基于震源机制的煤矿采动主应力场反演分析
李守锋,屈英
(华亭煤业集团华亭煤矿,甘肃华亭744100)
摘要:矿并岩体应力场属性是冲击地压防治需考虑的重要因素,而开采扰动可使原岩应力场变异,故在掌握原岩应力场属性的同时,应用囊源机制解答方法,以华亭煤矿250104工作面回采、250105工作面掘进时55个强度较高、震相清晰的矿震为基础,对矿井采动应力释放规律进行反演,分析了矿井采动应力场及其演化过程,进而反映受采动影响矿井应力场的调整和再平衡过程,并通过与现场地应力测量结果比较,认清矿井冲击地压发生机理,采取针对性较强的冲击地压防治措施,有效减轻了矿井冲击地压灾害。
关键词:应力场;矿囊:震源机制;反演;冲击地压
中图分类号:TD324
文献标志码:B
Inversion Analysis of Principal Stress Field of Coal Mining Based on Focus Mechanism
LI Shoufeng , QU Ying
( Huating Coal Mine, Huating Coal Indarstry Group, Huating 744100, China)
Abstract : The property of stress field of mine rock mass is an important factor which should be considered for prevention and control of rock burst. The mining disturbance can make the original rock stress field vary. Therefore, in mastering the property of the original rock stress field, the solution method of focus mechanism was applied,based on 55 strong mining shocks with relatively high intensity and clear seismic phase, which produced in the mining of 250104 working face and tunneling of 250105 working face in Huating Coal Mine, the stress release rule of mine mining was reversed, the mine mining stress field and its evolution process was analyzed. Furthermore, it reflected the adjustment and rebalancing process of mining stress field affected by mining, and by comparing with the results of site stress measurement, the mechanism of rock burst in mine was understand. The targeted measures to prevent and control the impact of rock burst were adopted, which effectively reduced the impact of rock burst in coal mine.
Keywords : stress field;mining shock ; focus mechanism; inversion;rock burst
震源(或破裂源)机制解答是研究大尺度岩体宏观破裂孕育和发生机理广泛使用的方法和途径。岩体破裂源研究始于美国的Ride,提出了“弹性回跳” 理论[1];随后Nakano进行了震源的定量研究[2]。这一领域在后来相当长时间内的研究方向,就是探累索用地震波初动符号和P、S波振幅比来确定与震源等价的点源类型和定向。但单个岩体破裂的破裂源机制反映的是破裂源处的应力释放特征,并不能完全反映应力场全貌,而众多岩体破裂源机制总体特征
收稿日期:2017-0731;2018-0412修订
作者简介:李守锋(1974一),男,甘肃静宁人,高级工程师,总工程师,主要从事煤矿技术管理及矿并灾害防治工作。 Email:314950273@qq.com。
· 90 万方数据
能够代表应力场的属性。
以往的研究未发现天然地震与采矿发生的矿震
震源机制存在系统和本质的差异,天然地震机制的绝大多数机理均可用于矿震,矿震破裂源机制的反演可以借鉴天然地震的反演方法。煤矿进人深部开采后,各种尺度矿震岩体破裂遍布矿井,其中一部分小尺度岩体破裂发生在采场附近演变为冲击地压或岩爆:一部分大尺度岩体破裂产生强弹性能释放(以下称强矿震),在全矿井甚至外围一定范围内分布[3-6]。矿震岩体破裂源是采动应力聚积与释放的策源地,破裂源的震源机制及其在时间、空间上的分布规律,可直接反映采动应力状态的演变。李铁等提出,煤矿采动卸荷重力应力场诱发作业突出了;张风鸣等提出,矿震的孕育和发生受到采动因素和区