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(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

Gamma ray computed tomography to evaluate wetting/drying soil structure changes

Texto completo
Autor(es):
Bacchi, O. O. S. ; Reichardt, K. ; Pires, L. F. [3]
Número total de Autores: 3
Tipo de documento: Artigo Científico
Fonte: NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIO; v. 229, n. 3-4, p. 443-456, Apr. 2005.
Área do conhecimento: Ciências Agrárias - Agronomia
Assunto(s):Física do solo   Umidade do solo   Porosidade do solo
Resumo

Wetting and drying (W-D) cycles can cause strong modifications of the structure of a soil, especially in pore distribution, which reflects the temporal and spatial distribution of soil water and, consequently, these processes can affect soil water and nutrient retention and movement. These alterations have important practical consequences when calculating soil water storages and matric potentials, widely used in irrigation management. The present paper has as objective to use gamma ray computed tomography (GCT) as a tool to investigate possible modifications in soil structure induced by W-D cycles and to analyze how these alterations can affect soil water retention. The GCT scanner used was a first generation system with a fixed source-detector arrangement, with a radioactive gamma ray source of 241Am. Soil samples were taken from profiles of three different soils characterized as Xanthic Ferralsol (Fx), Eutric Nitosol (Ne) and Rhodic Ferralsol (Fr). Eighteen samples (50 cm3), six from each soil, were submitted to none (T0), three (T1) and nine (T2) wetting/drying cycles. Based on image analysis it was possible to detect modifications in soil structure in all samples after wetting/drying cycles for all treatments. Tomographic unit profiles of the samples permitted to identify an increase on soil porosity with the increase in the number of wetting/drying cycles and it was also possible to quantify the average porosity values. The statistical test (Duncan test) indicates that there are significant differences between treatments for all samples at the 5% significance level. (AU)

Processo FAPESP: 02/05066-5 - Imagens microtomográficas e micromorfológicas na análise de mudanças estruturais do solo durante obtenção da curva de retenção da água no solo
Beneficiário:Luiz Fernando Pires
Modalidade de apoio: Bolsas no Brasil - Doutorado