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Automatic Framework for Extraction and Characterization of Wetting Front Propagation Using Tomographic Image Sequences of Water Infiltrated Soils

机译:使用渗水土壤的层析图像序列提取和表征湿润前传播的自动框架

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摘要

This paper presents a new automatic framework for extracting and characterizing the dynamic shape of the 3D wetting front and its propagation, based in a sequence of tomographic images acquired as water (moisture) infiltrates in unsaturated soils. To the best of the authors’ knowledge, the shape of the 3D wetting front and its propagation and progress over time has not been previously produced as a whole by methods in existing literature. The proposed automatic framework is composed two important and integrated modules: i) extraction of the 3D wetting front, and ii) characterization and description of the 3D wetting front to obtain important information about infiltration process. The 3D wetting front surface is segmented from 3D CT imagery provided as input via a 3D stochastic region merging strategy using quadric-regressed bilateral space-scale representations. Based on the 3D segmentation results, the normal directions at local curvature maxima of the wetting front surface are computed for 3D images of soil moisture, and its propagation is analyzed at the local directions in sites of maximal water adsorption, and described using histograms of curvature changes over time in response to sample saturation. These curvature change descriptors provide indirect measurements of moisture infiltration in soils, and soil saturation. Results using a field tomograph equipment specific for soil studies are encouraging, and suggest that the proposed automatic framework can be applied to estimate the infiltration of water in soils in 3D and in time.
机译:本文基于在水分(水分)渗入非饱和土壤中获得的一系列断层图像,提出了一种新的自动框架,用于提取和表征3D湿润前沿及其传播的动态形状。据作者所知,3D湿润前沿的形状及其随时间的传播和发展以前并未通过现有文献中的方法作为一个整体来产生。所提出的自动框架由两个重要且集成的模块组成:i)3D润湿前沿的提取,ii)3D润湿前沿的表征和描述,以获得有关渗透过程的重要信息。从3D CT图像中分割出3D润湿前表面,该图像是使用二次回归双边空间比例表示法通过3D随机区域合并策略作为输入提供的。根据3D分割结果,计算土壤水分的3D图像的润湿前表面局部曲率最大值处的法线方向,并分析在最大吸水部位局部方向上的传播,并使用曲率直方图进行描述随样品饱和而随时间变化。这些曲率变化描述符可间接测量土壤中的水分渗透和土壤饱和度。使用专门用于土壤研究的现场层析成像设备获得的结果令人鼓舞,并且表明所建议的自动框架可用于估计3D并及时地渗入土壤中的水。

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