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Computed X-ray tomography images of dry undisturbed soil samples of the coarse sandy loam of Korkusova Hut (KH) and the fine sand of Hupselse Beek (HB) are analysed concerning the image resolution, the direction of scanning and the evaluation of boundaries between the fast and slow flow domains. The image resolution appears to be a less important factor than the direction of scanning. Additional data...
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