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OVERBURDEN STRATA DEFORMATION MONITORING BASED ON DISTRIBUTED OPTICAL FIBER SENSING: NOVEL METHOD FOR GROUND CONTROL

机译:基于分布式光纤感测的覆盖层层变形监测:地面控制的新方法

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Overburden strata deformation monitoring is one of the key problems in ground control. Using geophysical method through surface drilling to detect strata deformation is commonly used in the industry. In this paper, a geophysical method based on the distributed optical fiber sensing (DOFS) system were conducted in the laboratory, where a DOFS-based strata deformation monitoring experiment was performed with three physical models. The results show that the DOFS method precisely detects the rock mass deformation and strata structure forming with the Brillouin frequency shifts (BFS) representation. The BFS curves are divided into three phases, which reflects the horizontal three zones developed in the overburden. The BFS distribution presents a multiple stages form, the 1st stage corresponds to the caving zone and the 2nd stage corresponds to the fracture zone. Based on the multiple stages form, the evolution of the water flowing through fractured zone have been determined and the controlling effect of key strata over the water flowing fracture has been pointed out. In the end, the comparison validation proves the accuracy and reliability of this method, and it could be a new approach for the ground control research.
机译:覆盖层层变形监测是地面控制中的关键问题之一。通过表面钻井使用地球物理方法来检测地层变形通常在工业中使用。本文在实验室进行了一种基于分布式光纤感测(DOFS)系统的地球物理方法,其中三种物理模型进行了基于DOF的地层变形监测实验。结果表明,DOFS方法精确地检测岩石质量变形和地层结构,与布里渊频率换档(BFS)表示形成。 BFS曲线分为三个阶段,这反映了在覆盖层中开发的水平三个区域。 BFS分布呈现多个阶段形式,第1级对应于腔区,第二级对应于裂缝区。基于多个阶段形式,已经确定了流过裂缝区的水的演变,并指出了钥匙地层对水流骨折的控制效果。最后,比较验证证明了这种方法的准确性和可靠性,它可能是地面控制研究的新方法。

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