巴拉素煤矿厚硬顶板地面压裂特性及防冲效果分析

Surface fracturing characteristics and anti-rock burst effect of thick and hard roof in Balasu Coal Mine

  • 摘要:
    目的 针对深部矿井厚硬顶板高强度开采易诱发冲击地压问题,以巴拉素煤矿2201工作面为工程背景,研究地面水平井压裂特性及防冲效果。
    方法 基于物理力学试验与脆性矿物分析,对目标岩层可压裂性进行判别,通过现场压裂测试获取岩层破裂压力及裂缝扩展特征,结合地面微震监测、巷道出水、矿压显现等多源数据对压裂效果进行验证。
    结果 确定煤层上方46.8 m处、厚度8.2 m的细砂岩层为主关键压裂层位,其具有强度大、可压裂性强和高脆性矿物含量;现场压裂测试得到破岩压力约为29 MPa,施工参数稳定可控;水力裂缝沿工作面走向呈带状分布,水平范围达262.6 m;压裂期间巷道出水增强,回采期间压裂区微震活动以小能量事件为主,周期来压步距明显减小。
    结论 地面水平井压裂可有效削弱厚硬顶板整体承载结构,使其由整体失稳向分级破断转化,从而实现冲击地压风险的区域性调控。

     

    Abstract: Aiming at the problem of rock burst induced by high-intensity mining of thick and hard roof in deep mines, the fracturing characteristics and anti-rock burst effect of surface horizontal wells were studied based on the engineering background of 2201 working face in Balasu Coal Mine. Based on physical and mechanical tests and brittle mineral analysis, the fracability of the target rock layer was discriminated. The fracture pressure and fracture propagation characteristics of the rock layer were obtained through field fracturing tests. The fracturing effect was verified by multi-source data such as surface microseismic monitoring, roadway water outlet and mine pressure appearance. It is determined that the fine sandstone layer with a thickness of 8.2 m at 46.8 m above the coal seam is the main key fracturing layer, which has high strength, strong fracability and high brittle mineral content. The field fracturing test shows that the rock breaking pressure is about 29 MPa, and the construction parameters are stable and controllable. The hydraulic fractures are distributed in a band along the strike of the working face, with a horizontal range of 262.6 m. During the fracturing period, the water outlet of the roadway is enhanced. During the mining period, the microseismic activity in the fracturing area is dominated by small energy events, and the periodic weighting step is significantly reduced. Surface horizontal well fracturing can effectively weaken the overall bearing structure of thick and hard roof, and make it transform from overall instability to graded breaking, so as to realize the regional control of rock burst risk.

     

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