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Coal Bumps in an Eastern Kentucky Coal Mine 1989 to 1997

机译:1989年至1997年在肯塔基州东部煤矿的爆煤事故

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Coal mines in southern West Virginia, south-western Virginia and eastern Kentucky have experienced coal bumps at least since 1933. Most of the bumps have occurred due to high cover, strong roof and floor strata and stress concentrations due to the mining sequence. A longwall mine in eastern Kentucky first experienced coal bumps on the tailgate side of the longwall face in 1989. The bumps continued until 1996. The bumps were the result of: 1 Thick overburden up to 2200 feet 2 Strong roof and floor (strata strengths up to 25,600 psi UCS and elasticity modulus up to 4,800,000 psi 3 Previous over-mining in places 4 Sandstone channels Not all characteristics occurred simultaneously. The bumps produced seismic events recorded up to 4.3 (Richter scale magnitude), and damaged pillars that were up to 147 by 152 feet in size. During the 8 years that the bumps occurred, a large quantity of data was obtained in an effort to develop methods to predict an event, and reduce or eliminate the bumps. 1 In-situ strength properties of floor, coal and roof strata 2 Lab testing of floor, coal and roof samples 3 Monitoring gate road pillar response with stress metres, extensometers and convergence stations 4 Shield leg response 5 Monitoring in an effort to determine precursors was conducted using a digital microseismic monitoring system. 6 Back calculation of gate road pillar strength A number of different remedies were trialed in an effort to eliminate or decrease the severity of the bumps. 7 The gate road longwall design was varied 1 Pillar size and shape 2 3 and 4 entry gate road designs 8 Water infusion in longwall panels, 9 Hydraulic induced face bumps, 10 Disruption of the roof strata A yield-abutment-yield pillar design was the most effective method in reducing the affect of bumps by moving the events onto the abutment pillars, but the bumps were never eliminated and adequate precursors and advanced warnings were never achieved.
机译:至少自1933年以来,西维吉尼亚州南部,维吉尼亚州西南部和肯塔基州东部的煤矿就经历了煤块颠簸。大部分颠簸的发生是由于高覆盖层,坚固的顶板和底板地层以及采矿顺序造成的应力集中。肯塔基州东部的一处长壁矿山于1989年首次在长壁工作面的后挡板侧经历了煤块撞击。这些撞击一直持续到1996年。这些撞击的结果是:1厚至2200英尺的厚覆盖层2坚固的顶板和底板(地层强度提高到25,600 psi UCS和高达4,800,000 psi的弹性模量3先前在某处的过度开采4砂岩通道并非所有特征同时发生,颠簸产生的地震事件记录高达4.3(Richter规模),损坏的支柱高达147尺寸为152英尺。在颠簸发生的8年中,获得了大量数据,以开发预测事件的方法,并减少或消除颠簸1地板,煤的原位强度特性和屋顶地层2地板,煤和屋顶样品的实验室测试3使用应力米,引伸计和会聚站监控门道支柱响应4盾构腿响应5确定是使用数字微震监测系统进行的。 6闸门路基强度的反算为了消除或减轻颠簸的严重程度,尝试了许多不同的补救措施。 7闸门长壁设计各不相同1支柱的尺寸和形状2 3和4入口闸门设计8长壁板中的注水,9液压引起的面撞,10顶板的破坏屈服-基台-屈服支柱设计是通过将事件移到基台支柱上来减少颠簸影响的最有效方法,但从来没有消除颠簸,也从未获得足够的前兆和预警。

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  • 会议地点 MorgantownWV(US)
  • 作者

    John Hoelle;

  • 作者单位

    U.S.National Institute for Occupational Safety and Health;

    West Virginia Coal Association;

    U.S.Mine Safety and Health Administration;

    West Virginia University;

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