首页> 外文会议>Multidisciplinary conference on sinkholes and the engineering and environmental impacts of karst >Monitoring soil void formation along highway subgrade using Time Domain Reflectometry (TDR), a pilot study at Guilin-Yangshuo highway, Guangxi, China
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Monitoring soil void formation along highway subgrade using Time Domain Reflectometry (TDR), a pilot study at Guilin-Yangshuo highway, Guangxi, China

机译:使用时域反射测量(TDR)监测沿高速公路路基的土壤空隙形成,中国广西桂林 - 阳朔高速公路试点研究

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Soil voids and sinkhole collapses are main geological hazards during highway construction in the karst regions of southwestern China. Controlled by karst development and groundwater fluctuation, soil void usually forms abruptly and then expands progressively until a sinkhole develops. The goal of this research is to develop a cost-effective and efficient method to monitor the soil void formation and propagation, which would potentially prevent and greatly reduce damages caused by future sinkhole collapses. Recent monitoring methods include Ground Penetrating Radar (GPR), inclinometers, Interferometric Synthetic Aperture Radar (InSAR), real-time water pressure monitoring in karst opening, the Brillouin Optical Time Domain Reflectometry (BOTDR), and Time Domain Reflectometry (TDR). The unique features of the BOTDR and TDR techniques such as distributed measurement, long distance range, high resolution, and remote monitoring make them more effective to monitor soil voids and sinkholes along highways in active karst area. Because of the high cost of the Optical Fiber Strain Analyzer, the equipment for BOTDR, TDR was used as a cost-effective method to monitor soil voids and sinkholes. In a pilot study, a 110 m section of subgrade along Guilin-Yangshuo highway was selected to establish a long-term monitoring site, where soil voids formed frequently and more than 43 voids were delineated by GPR. Five lines of coaxial cables were installed on the surface of the subgrade. These lines were parallel to the main axis of the highway with a 3 m separation interval in between. A monitoring station was established on December 21, 2006, and soil deformation measurements were recorded monthly. In addition, water pressure in karst opening was monitored by piezometer and precipitation was recorded by rain gauge at the station. Results of the monitoring measurements show no major subgrade deformation in the past 10 months. One cable fault caused by construction truck was detected by TDR. One minor cable fault caused by subsurface voids or uneven subsidence during construction was detected. Further testing or GPR scan are needed to interpret the minor cable fault.
机译:土壤空隙和污水坍塌是中国西南喀斯特地区公路建设期间的主要地质灾害。由喀斯特开发和地下水波动控制,土壤空隙通常突然形成,然后逐步扩展,直到污水孔发育。该研究的目标是开发一种成本效益和有效的方法,以监测土壤空隙形成和传播,这可能会阻止并大大减少未来污水坍塌造成的损害。最近的监测方法包括地面穿透雷达(GPR),倾角系,干涉式合成孔径雷达(INSAR),在岩溶开口中,布里渊光学时域反射区(BOTDR)和时域反射率(TDR)。 BOTDR和TDR技术的独特特征,如分布式测量,长距离范围,高分辨率和远程监测,使其更有效地监测有源岩溶区域的高速公路的土壤空隙和下沉孔。由于光纤应变分析仪的高成本,BOTDR,TDR的设备被用作监测土壤空隙和下沉孔的成本效益的方法。在试点研究中,选择了沿桂林 - 阳朔公路110米的路基分布,建立长期监测点,其中经常形成的土壤空隙率为GPR划分。在路基的表面上安装了五条同轴电缆。这些线平行于高速公路的主轴,在其间具有3米的分离间隔。 2006年12月21日建立了一个监测站,每月记录土壤变形测量。此外,通过压阻计监测岩溶开口的水压,并通过电站的雨量计记录沉淀。监测测量结果显示过去10个月内没有大规模的路基变形。由TDR检测由施工卡车引起的一个电缆故障。检测到施工期间由地下空隙或不均匀沉降引起的一个次要电缆故障。需要进一步测试或GPR扫描来解释次要电缆故障。

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