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Site Investigation and Analyses of Landslide Range Using Particle Image Velocimetry

机译:利用粒子图像测速技术进行滑坡范围的实地调查与分析。

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In order to understand the stability and slipping behavior of the slope, in situ investigation and monitoring have been carried out at 12.3 K of Nantou County 89th County Road, Taiwan. The acquired potential sliding depth and range of moving area from the boring logs and inclinometer measurements match with the outcomes from electrical resistivity tomography. The other purpose of this study was to obtain the horizontal displacement field of the landslide at station 12.3 K's landslide and its surrounding area using the particle image velocimetry (PIV) technique. The orthophotographs, taken during 2008 and 2012, were analyzed using the PIVview2C. The results show that the maximum horizontal displacement is about 5.5 to 6.1 m in this study area. For movements in 2008-2009 and 2010-2012, the major displacement is around 5 to 6.5 m. Most of the calculated displacement magnitudes are less than 2.5 m in 2009-2010. The major moving direction is toward the azimuth 247.5°-292.5°. The results of PIV analysis can quickly identify the major moving zones and displacement fields compared with traditional methods.
机译:为了了解边坡的稳定性和滑移特性,在台湾南投县第89县道12.3 K进行了现场调查和监测。通过钻孔测井和测斜仪测量获得的潜在滑动深度和移动区域范围与电阻层析成像的结果相匹配。这项研究的另一个目的是使用粒子图像测速(PIV)技术获得驻地12.3 K滑坡及其周围区域的滑坡水平位移场。使用PIVview2C分析了2008年和2012年拍摄的正射照片。结果表明,该研究区域的最大水平位移约为5.5至6.1 m。对于2008-2009年和2010-2012年的运动,主要位移约为5至6.5 m。在2009-2010年间,大多数计算出的位移量小于2.5 m。主要运动方向是朝向方位角247.5°-292.5°。与传统方法相比,PIV分析的结果可以快速识别主要的运动区域和位移场。

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