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Non-destructive image analysis of soil surface porosity and bulk density dynamics

2010; Elsevier BV; Volume: 80; Issue: 4 Linguagem: Inglês

10.1016/j.radphyschem.2010.12.006

1879-0895

Luiz F. Pires, Fabio Augusto Meira Cássaro, Osny Oliveira Santos Bacchi, Klaus Reichardt,

Geophysical Methods and Applications

A gamma-ray computed tomography (CT) scanner was used to evaluate changes in the structure of clayey soil samples with surface compaction submitted to wetting and drying (W–D) cycles. The obtained results indicate that W–D cycles promoted an increasing of about 10% in soil porosity with a decreasing of about 6% in soil bulk density of this compacted region. With the use of the CT it was also possible to define the thickness of the compacted region that in our case was of about 8.19 mm. This last information is very important, for instance, to estimate hydraulic parameters in infiltration models. Finally, CT analysis showed that the compacted region remained at the surface samples, even after the application of the W–D cycles.