1887

Abstract

Soil cracks, whose formation are associated to natural climate phenomena such as swelling and shrinking, play an important role in water and gas transfers. Up to now, their 3D structure was characterised either by serial sections (Cousin, 1996) which is a destructive technique or X-ray tomography (Macedo et al., 1998), which is applicable on limited size sample.

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/content/papers/10.3997/2214-4609.201414588
2003-09-01
2024-04-26
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