基于GNSS的综采工作面地表移动变形监测与规律研究

Surface movement deformation monitoring and law of fully mechanized mining face based on GNSS

  • 摘要: 【目的】为探究煤层开采诱发的地表移动变形规律,【方法】以某矿132201工作面为工程背景,通过设立GNSS连续监测系统进行地表移动变形数据的现场实测。本研究在采区边缘设立了基准点,并定期进行水准测量与GNSS高程校正,同时在采空区外围确保不会发生沉降的稳定区域埋设了3个水准基准点,并在预计沉陷范围外设置GNSS基准站对开采期间的地表沉降变形进行自动实时监测。观测站设计采用高效的线性布局,共设置4个GNSS监测点(GP1~GP4)以捕捉工作面开采过程中顶板覆岩的变形动态。【结果】监测结果显示,地表移动过程历经启动、活跃至衰退3个阶段,各阶段特征鲜明,分别体现了地表响应的初始、加速与稳定过程。随着工作面的推进,上覆岩层运动已波及地表,下沉盆地范围不断扩大,地表下沉程度加剧。分析表明,地表移动变形的复杂性源于多因素综合作用,包括开采宽度、推进速率、煤层厚度、开采深度以及地表覆盖层性质等。这些因素相互交织,共同决定了地表沉降的时空分布与强度变化。【结论】本研究不仅揭示了研究区当前的地表变形状态,还通过趋势预测为类似矿区提供了科学预测与控制地表移动变形的策略框架。这些发现不仅丰富了采矿地质工程领域的理论知识,也为实际生产中的安全高效开采提供了重要的技术支撑与决策依据。

     

    Abstract: In order to explore the surface movement deformation characteristics of coal seam mining, this paper takes the 132201 working face as the background of the project, and conducts the on-site measurement of the surface movement deformation data by setting up a continuous monitoring system of GNSS.The study set up reference points at the edge of the mining area, and regularly carried out level surveys and GNSS elevation corrections, while three level reference points were buried in the stable area on the periphery of the mining area to ensure that no subsidence would occur as the starting point of level surveys.A GNSS reference station was also set up outside the expected subsidence range to automatically monitor the surface subsidence and deformation in real time during the mining period.The station design adopts an efficient linear layout, with a total of four GNSS monitoring points(GP1 to GP4) to capture the deformation dynamics of the roof overburden during the working face mining process.The monitoring results show that the surface movement process has gone through three stages of initiation, activity to decline, and each stage has distinctive characteristics, reflecting the initial, accelerated and stable process of the surface response, respectively.As the working face advances, the movement of the overlying rock strata has spread to the surface, the subsidence basin is expanding and the degree of surface subsidence is intensifying.Analyses show that the complexity of surface movement and deformation stems from the combined effect of multiple factors, including mining width, advance rate, coal seam thickness, mining depth and the nature of the surface overburden.These factors are intertwined with each other and jointly determine the spatiotemporal distribution and intensity changes of surface subsidence.Based on the detailed subsidence, displacement and deformation data, this study not only reveals the current state of surface deformation in the study area, but also provides a strategic framework for scientific prediction and control of surface movement and deformation in similar mining areas through trend prediction.

     

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