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Formation process and mechanism of seepage channels around grout curtain from microseismic monitoring: A case study of Zhangmatun iron mine, China

机译:微震监测灌浆窗帘周围渗流通道的形成过程和机制 - 以张马洪铁矿,中国

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摘要

The grout curtain in Zhangmatun iron mine, China, suffers from the leakage of water due to the influence of multiple factors including inadequate grouting area, weak rock and mining disturbance. Water seepage through rock mass around the grout curtain further deteriorates the water plugging'effect of the grout curtain and poses a potential hazard to workers underground. Thus, a microseismic (MS) monitoring system was established in the Zhangmatun iron mine. In the present paper, a MS monitoring analysis method for assessing a potential seepage channel is proposed. Using the proposed MS monitoring analysis method, the dip, dip angle and center depth of the potential seepage plane across the grout curtain in Zhangmatun iron mine are determined to be 126.1 degrees E, 53.97 degrees and 275 m, respectively. The spatial and temporal behaviors of density distribution, source parameters and cracking type of the seismic source are analyzed to reveal the initiation, propagation, coalescence of seepage channel located at the southwest of the iron mine. Four types of local seepage channel formation, processes are summarized by correlating the mechanism of microcracking. Two main weak areas around the grout curtain at the levels of 230 m and 318 m are identified and two seepage paths whose water discharge points are localized to the roof of stope 9, 10 and sidewall of stope 10 are determined, respectively. Our study helps to get a better understanding of damage and failure of rock mass around grout curtain and thus provides a basis for taking reinforcement measures to secure the stability of grout curtain in mines.
机译:中国张马洪铁矿的灌浆窗帘由于多种因素的影响而遭受了水的泄漏,包括灌浆面积不足,岩石和采矿障碍。水渗漏通过岩块围绕灌浆窗帘进一步恶化了灌浆窗帘的水堵塞,对工人造成了潜在的危险。因此,在张马洪铁矿中建立了微震(MS)监测系统。在本文中,提出了一种用于评估潜在渗流通道的MS监测分析方法。利用所提出的MS监测分析方法,张门屯铁矿灌浆窗帘潜在渗流平面的浸渍,倾角和中心深度分别为126.1摄氏度,53.97度和275米。分析了地震源的密度分布,源参数和开裂类型的空间和时间行为,揭示了位于铁矿西南部的渗流通道的启动,传播,渗流。通过关联微裂纹机制来概述四种类型的本地渗流通道形成。围绕灌浆窗帘周围的两个主要弱区域,分别确定水排放点的两个渗流路径,其排水点置于迹象9,10和侧壁的侧壁10和侧壁的侧壁10。我们的研究有助于更好地了解灌浆窗帘周围岩石块的损坏和失败,从而为采取加强措施来确保矿山灌浆窗帘的稳定性提供了基础。

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