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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:使用时域反射仪(TDR)监测公路路基上的土壤空洞形成,这是在中国广西桂林至阳朔高速公路上进行的一项初步研究

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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:在西南喀斯特地区的公路建设过程中,土壤空隙和塌陷塌陷是主要的地质灾害。受岩溶发育和地下水波动的控制,土壤孔隙通常会突然形成,然后逐渐扩展,直至形成下陷。这项研究的目的是开发一种经济有效的方法来监测土壤中空洞的形成和传播,这将有可能防止并大大减少由未来的塌陷造成的破坏。最近的监测方法包括探地雷达(GPR),测斜仪,干涉合成孔径雷达(InSAR),岩溶洞实时实时水压监测,布里渊光学时域反射仪(BOTDR)和时域反射仪(TDR)。 BOTDR和TDR技术的独特功能(例如分布式测量,长距离范围,高分辨率和远程监控)使它们更有效地监控活动喀斯特地区公路沿线的土壤空洞和塌陷。由于光纤应变分析仪的高昂成本,BOTDR,TDR的设备被用作一种经济有效的方法来监测土壤孔隙和下沉孔。在一项试点研究中,沿桂阳高速公路的路基110 m断面被选作长期监测点,该处土壤空洞频繁形成,GPR划定了43个以上的空洞。五层同轴电缆安装在路基表面。这些线与高速公路的主轴线平行,且两者之间的间隔为3 m。 2006年12月21日建立了监测站,每月记录土壤变形测量值。另外,岩溶开口处的水压通过压力计监测,并通过雨量计记录站内的降水。监测结果表明,在过去的10个月中,路基没有大的变形。 TDR检测到一辆由工程车引起的电缆故障。在施工过程中,发现了由地下空隙或不均匀沉降引起的一小段电缆故障。需要进一步的测试或GPR扫描来解释次要电缆故障。

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