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Using a Parallel Helical Sensing Cable for the Distributed Measurement of Ground Deformation

机译:使用平行螺旋传感电缆进行地面变形的分布式测量

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摘要

Surface and underground stretched deformation is one of the most important physical measurement quantities for geological-disaster monitoring. In this study, a parallel helical sensing cable (PHSC) based on the time-domain reflectometry (TDR) technique is proposed and used to monitor large ground stretched deformation. First, the PHSC structure and manufacturing process are introduced, and then, distributed capacitance, distributed inductance, and characteristic impedance were derived based on the proposed stretched-structure model. Next, the relationship between characteristic impedance and stretched deformation was found, and the principle of distributed deformation measurement based on the TDR technique and PHSC characteristic impedance was analyzed in detail. The function of the stretched deformation and characteristic impedance was obtained by curve fitting based on the theoretically calculated results. A laboratory calibration test was carried out by the designed tensile test platform. The results of multi-point positioning and the amount of stretched deformation are presented by the tensile test platform, multi-point positioning measurement absolute errors were less than 0.01 m, and the amount of stretched deformation measurement absolute errors were less than 3 mm, respectively. The measured results are in good agreement with the theoretically calculated results, which verify the correctness of theoretical derivation and show that a PHSC is very suitable for the distributed measurement of the ground stretched deformation.
机译:表面和地下拉伸变形是地质灾害监测最重要的物理测量量之一。在该研究中,提出了一种基于时域反射仪(TDR)技术的平行螺旋感测电缆(PHSC)并用于监测大地拉伸变形。首先,引入PHSC结构和制造工艺,然后基于所提出的拉伸结构模型导出分布式电容,分布式电感和特性阻抗。接下来,发现了特征阻抗和拉伸变形之间的关系,并详细分析了基于TDR技术和PHSC特征阻抗的分布式变形测量的原理。通过基于理论计算结果,通过曲线拟合获得拉伸变形和特征阻抗的函数。通过设计的拉伸试验平台进行实验室校准测试。多点定位和拉伸变形量的结果由拉伸试验平台提出,多点定位测量绝对误差小于0.01μm,并且拉伸变形测量绝对误差的量分别小于3mm 。测量结果与理论计算结果良好,验证了理论推导的正确性,并表明PHSC非常适合于地面拉伸变形的分布测量。

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