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Numerical analysis of longwall mining layout for a Wyoming Trona mine

机译:怀俄明州Trona矿长壁开采布局的数值分析

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At Solvay Mine, located in southwestern Wyoming, a subhorizontal trona seam is mined at depths of between 460 and 490 m using mechanized room-and-pillar and longwall mining methods. The stratigraphy at the mine generally consists of horizontally laminated (i.e., bedded) sedimentary rocks comprised mostly of shales and sandstones with significantly contrasting mechanical properties. Most notably, a 43-82 m-thick massive, brittle sandstone unit (Tower Sandstone), located approximately 100 m above the mining level, has a tendency to promote stress arching within the overburden rock that can bridge over panel-scale mine instabilities and can lead to violent multi-panel collapse failure. One such violent collapse is the 5.1 magnitude seismic event due to a 1 x 2 km multi-panel failure on February 3, 1995. It has proven difficult to account for this arching behavior with conventional mine design methods, such as the tributary area method. Therefore, over the past two decades or more, Solvay Mine has been utilizing numerical modeling techniques along with field instrumentation/monitoring as part of an integrated program to gain an enhanced understanding of the complex response of the overlying stratigraphy (i.e., arching) to mining. In 2005 and 2006, several longwall panels in the northwest and southeast areas of the mine were instrumented and monitored during mining. Two- and three-dimensional numerical models were developed and calibrated on the basis of the instrumentation data, and these models were then used for mine design verification (e.g., pillar and panel dimensions). This mining case study illustrates the complex excavation response due to the contrasts in stratigraphy at Solvay Mine and presents a numerical modeling study that captures the dominant aspects of these conditions. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在怀俄明州西南部的Solvay矿,使用机械化的房柱和长壁开采方法在460至490 m的深度开采了水平水平的天然碱煤层。矿山地层通常由水平层压(即层状)的沉积岩组成,这些沉积岩主要由页岩和砂岩组成,具有明显不同的力学性能。最值得注意的是,位于开采水平上方约100 m的43-82 m厚的块状脆性砂岩单元(塔式砂岩)具有促进覆岩内应力拱起的趋势,这种应力拱起可以弥合面板规模的矿山不稳定性和会导致剧烈的多面板崩溃失败。 1995年2月3日由于1 x 2 km的多面板破坏导致的5.1级地震事件就是这样的剧烈倒塌。事实证明,用传统的矿山设计方法(例如支流面积法)很难解释这种拱形行为。因此,在过去的二十多年或更久的时间里,索尔维矿山一直将数值建模技术与现场仪表/监测技术结合起来,作为集成程序的一部分,以加深对上层地层(即拱形)对采矿的复杂响应的理解。 。在2005年和2006年,在采矿过程中对矿井西北和东南地区的几个长壁板进行了检测和监控。根据仪器数据开发并校准了二维和三维数值模型,然后将这些模型用于矿山设计验证(例如,支柱和面板尺寸)。该采矿案例研究说明了由于索尔维矿层地层差异而引起的复杂开挖响应,并提出了一个数值模型研究,该研究涵盖了这些条件的主要方面。 (C)2016 Elsevier Ltd.保留所有权利。

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