黏土三维计算机断层成像中孔隙网络和含水量分布的测定

Anton W J Heijs, Jacqueline de Lange
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引用次数: 7

摘要

通过分析土壤中水分分布的三维图像,可以提高对多孔介质流动的认识。我们报告了这样一项研究,使用计算机断层扫描(CT)首先在干燥条件下扫描粘土样品。然后,在渗透实验后,通过在潮湿条件下再次扫描样品。我们使用测试幻影来确定最佳扫描参数,以获得具有高对比度和小标准差的双峰灰度值分布的图像。我们还确定了切片厚度和重建算法对图像恢复和分割的影响。为了获得孔隙空间的良好三维表示,我们以1 mm的轴向分辨率和0.27 × 0.27 mm2的像素尺寸相邻扫描切片。孔隙中的空气和粘土背景之间的高对比度允许对分割进行全局阈值设定,从而保留孔隙网络的连通性和拓扑结构。根据干样和湿样图像的差异,确定了水的含量分布。利用图像数据进行水分布测量,研究孔隙网络结构与水流的关系。
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Determination of pore networks and water content distributions from 3-D computed tomography images of a clay soil

Knowledge of flow in porous media can be improved by analyzing three-dimensional (3-D) images of the water distribution in a soil. We report on such a study using computed tomography (CT) scanning of a clay soil sample first in dry conditions. Then, after an infiltration experiment, by scanning the sample again in wet conditions. We used test phantoms to determine the optimal scanning parameters to obtain images with a bimodal gray value distribution with high contrast and small standard deviation. We also determined the effect of slice thickness and reconstruction algorithm on the restoration and segmentation of the images. For a good 3-D representation of the pore space we scanned the slices adjacently at an axial resolution of 1 mm and a pixel size of 0.27 × 0.27 mm2. The high contrast between air in the pores and the clay background allowed a global thresholding for the segmentation whereby the connectivity and topology of the pore networks is conserved. From the difference between the images of the dry sample and the wet sample we determined the water content distribution. We used the image data for measurements of the water distribution to study the relation between the structure of the pore networks and water flow.

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