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Transparent Sand Experimental Method for Geotechnical Physical Modeling Using Digital Imaging of Particle Image Velocimetry

机译:基于粒子图像测速数字成像的岩土物理建模透明砂实验方法

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摘要

By means of the technology of particle image velocimetry (PIV), the physical modelings, using transparent sand and natural sand, were set up to simulate the shallow foundation, respectively. The transparent soil is composed of fused quartz and correspondingly refractive index-matched flammable liquid. The flammable liquid is blended by two white mineral oils, Krystol40 and Puretol7. Transparent sand model was projected by a laser light sheet; meanwhile, the digital images of soil deformations caused by shallow foundation were captured. The PIV was employed to obtain the generated displacement fields from the digital images. The experimental results indicate that the deformation trends in transparent sand model are consistent with that in natural Ottawa sand model; however, the influential region is expanded by about 1.5 times, and the zone and magnitude of down-drag subsidence are extremely enlarged in transparent soil model, compared with those in Ottawa sand model. The verification of test results shows that the shallow strain path method is not suitable for the small-scale transparent sand and natural sand models.
机译:借助粒子图像测速技术(PIV),分别建立了使用透明砂和天然砂的物理模型来模拟浅层基础。透明土壤由熔融石英和相应的折射率匹配的易燃液体组成。易燃液体与两种白色矿物油Krystol40和Puretol7混合。透明砂模型由激光片投影;同时,获取了由浅层基础引起的土壤变形的数字图像。使用PIV从数字图像中获取生成的位移场。实验结果表明,透明砂模型的变形趋势与天然渥太华砂模型的变形趋势一致。然而,与渥太华砂土模型相比,透明土模型的影响范围扩大了约1.5倍,下沉沉降的区域和幅度极大地增加了。测试结果的验证表明,浅应变路径法不适用于小型透明砂和天然砂模型。

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