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Three-Dimensional Quantification of Intra-Aggregate Pore-Space Features using Synchrotron-Radiation-Based Microtomography

机译:使用基于同步辐射的显微断层摄影术对聚集体内部孔隙空间特征进行三维量化

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Pore network geometries of intra-aggregate pore spaces are of great importance for water and ion flux rates controlling C sequestration and bioremediation. Advances in non-invasive three-dimensional imaging techniques such as synchrotron-radiation-based x-ray microtomography (SR-µCT), offer excellent opportunities to study the interrelationships between pore network geometry and physical processes at spatial resolutions of a few micrometers. In this paper we present quantitative three-dimensional pore-space geometry analyses of small scale (5 mm across) soil aggregates from different soil management systems (conventionally tilled vs. grassland). Reconstructed three-dimensional microtomography images at approximate isotropic voxel resolutions between 3.2 and 5.4 µm were analyzed for pore-space morphologies using a suite of image processing algorithms associated with the software published by Lindquist et al. Among the features quantified were pore-size distributions (PSDs), throat-area distributions, effective throat/pore radii ratios as well as frequency distributions of pore channel lengths, widths, and flow path tortuosities. We observed differences in storage and transport relevant pore-space morphological features between the two aggregates. Nodal pore volumes and throat surface areas were significantly smaller for the conventionally tilled (Conv.T.) aggregate (mode 7.9 x 10–7 mm3/ 63 µm2) than for the grassland aggregate (mode 5.0 x 10–6 mm3/ 400 µm2), respectively. Path lengths were shorter for the Conv.T. aggregate (maximum lengths < 200 µm) compared with the grassland aggregate (maximum lengths > 600 µm). In summary, the soil aggregate from the Conv.T site showed more gas and water transport limiting micromorphological features compared with the aggregate from the grassland management system.
机译:聚集体内孔隙空间的孔网络几何形状对于控制C螯合和生物修复的水和离子通量速率非常重要。非侵入式三维成像技术的发展,例如基于同步辐射的X射线显微断层照相术(SR-µCT),为在几微米的空间分辨率下研究孔网几何结构与物理过程之间的相互关系提供了极好的机会。在本文中,我们介绍了来自不同土壤管理系统(常规耕作与草地)的小规模(5毫米宽)土壤团聚体的三维孔空间几何定量分析。使用与Lindquist等人发布的软件相关联的一组图像处理算法,分析了在3.2和5.4 µm之间近似各向同性体素分辨率的重建的三维显微断层扫描图像的孔隙空间形态。量化的特征包括孔径分布(PSD),喉道面积分布,有效喉道/孔半径比以及孔道长度,宽度和流路曲折的频率分布。我们观察到两种聚集体之间在存储和运输相关的孔隙空间形态特征方面的差异。传统耕作(Conv.T.)骨料(模式为7.9 x 10–7 mm3 / 63 µm2)的节点孔体积和喉部表面积要比草地骨料(5.0 x 10–6 mm3 / 400 µm2的模式)小得多。 , 分别。 Conv.T.的路径长度较短骨料(最大长度> 600 µm)与草料(最大长度<600 µm)相比。总之,与草地管理系统的土壤团聚体相比,Conv.T站点的土壤团聚体显示出更多的气水运移限制了微观形态特征。

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