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Measurement of Soil Shrinkage Curve Using Photogrammetry

机译:摄影测量法测量土壤收缩曲线

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Photogrammetry techniques have been widely used in geotechnical engineering both in the field and laboratory. In this study, photogrammetry is used to determine the shrinkage curves of an expansive soil. The shrinkage curve is a plot of volume of soil with water content as a soil dries. While, it is relatively easy to determine the gravimetric water content during drying, it is difficult to determine the volume of the soil specimen during drying. Using photogrammetry, the volumetric change of a soil specimen can be obtained by constructing a 3D model of the soil specimen using 2D images at various times. The difference in volumes of the soil specimen between two different times gives the volumetric change. Unlike previous studies, low-cost camera, and freeware are used to make the proposed method easily accessible. Moreover, this approach is non-contact and non-destructive and hence the soil specimen remains undisturbed during drying. In this study, a novel setup is developed which allows a handphone camera to move 360° around the soil specimen for capturing images. Considerations in the setup include lighting, number of images, and camera position. Proper lighting is essential to avoid shadow and distortion in the 3D model. A minimum number of images are required to ensure that the 3D model is constructed successfully. The camera can be fixed at one orientation (elevation and tilt). Two different handphone cameras of different specifications are evaluated. It is observed that 5-megapixel and 8-megapixel cameras gave similar results which show that camera having lower specification (5-megapixel) can be used to obtain an accurate volume measurement of the soil specimen. The absolute error in volume determination given by the two handphone cameras is about 0.3%. Generally, the volume of soil specimen with asymmetric deformation can be determined more accurately by photogrammetry compared to the conventional method.
机译:摄影测量技术已在现场和实验室中广泛用于岩土工程中。在这项研究中,摄影测量法用于确定膨胀土的收缩曲线。收缩曲线是随着土壤干燥而具有水含量的土壤体积的图。尽管在干燥过程中确定重量水含量相对容易,但在干燥过程中确定土壤样品的体积却很困难。使用摄影测量法,可以通过在不同时间使用2D图像构建土壤标本的3D模型来获得土壤标本的体积变化。在两个不同时间之间土壤样品的体积差异给出了体积变化。与以前的研究不同,低成本照相机和免费软件被用来使所提出的方法易于使用。而且,这种方法是非接触的和非破坏性的,因此土壤样品在干燥过程中保持不受干扰。在这项研究中,开发了一种新颖的装置,该装置可以使手机摄像头围绕土壤样本移动360°以捕获图像。设置中的注意事项包括照明,图像数量和相机位置。适当的照明对于避免3D模型中的阴影和变形至关重要。需要最少数量的图像以确保成功构建3D模型。可以将相机固定在一个方向(仰角和仰角)。对两个不同规格的手机摄像头进行了评估。可以看出,5百万像素和8百万像素相机给出了相似的结果,表明具有较低规格(5百万像素)的相机可用于获得土壤样品的准确体积测量值。两个手机摄像头给出的音量确定的绝对误差约为0.3%。通常,与常规方法相比,通过摄影测量法可以更精确地确定具有不对称变形的土壤样本的体积。

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