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Quantification of soil shrinkage in 2D by digital image processing of soil surface

机译:通过土壤表面数字图像处理量化二维土壤收缩

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摘要

Knowledge of soil shrinkage behavior is needed to improve the understanding and prediction of changes of unsaturated hydraulic properties in non-rigid soils. The heterogeneity and interaction of horizontal and vertical soil shrinkages that produce soil cracks and associated soil subsidence require additional quantification. Vertical shrinkage can be calculated easily by soil height with vernier caliper. However, a quantitative and feasible measurement of horizontal shrinkage has not been developed yet because of the complicated and irregular geometry of soil cracks. This paper introduces a new method to measure soil cracks non-destructively and continuously by digital image analysis. Using Adobe Photoshop and Windows Scion 4.02 image processing, theproposed procedure accurately identifies changes as small as 1.0 mm2 and shows differences even when areas of soil cracks were increased by as little as 1%. Various geometry factor values indicated soil shrinkage in the two dimensions was anisotropic during the whole drying. During initial dehydration from saturation, only subsidence shrinkage could be identified. With the further dehydration, the soil cracks developed and increased in size. These results suggest that the heterogeneity of soil shrinkage in 2D should be taken into account when modeling the total soil shrinkage behavior and associated unsaturated hydraulic properties.
机译:需要了解土壤的收缩行为,以增进对非刚性土壤中非饱和水力特性变化的理解和预测。产生土壤裂缝和相关的土壤沉降的水平和垂直土壤收缩的异质性和相互作用需要额外的量化。垂直收缩率可以很容易地用游标卡尺通过土壤高度来计算。然而,由于土壤裂缝的几何形状复杂且不规则,因此尚未开发出定量且可行的水平收缩率测量方法。介绍了一种通过数字图像分析无损连续测量土壤裂缝的新方法。通过使用Adobe Photoshop和Windows Scion 4.02图像处理,所建议的过程可以准确地识别出小至1.0 mm2的变化,即使土壤裂缝的面积仅增加了1%,也能显示出差异。各种几何因子值表明在整个干燥过程中二维土壤收缩是各向异性的。在最初的饱和脱水过程中,只能识别出沉降收缩。随着进一步的脱水,土壤裂缝发展并增大。这些结果表明,在对总土壤收缩行为和相关的不饱和水力特性进行建模时,应考虑二维土壤收缩的非均质性。

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