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(Reference retrieved automatically from SciELO through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

The use of gamma ray computed tomography to investigate soil compaction due to core sampling devices

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Author(s):
Luiz F. Pires [1] ; Robson C. J. Arthur [2] ; Vladia Correchel [3] ; Osny O. S. Bacchi [4] ; Klaus Reichardt [5] ; Rene P. Camponez do Brasil [6]
Total Authors: 6
Affiliation:
[1] Universidade de São Paulo. Centro de Energia Nuclear na Agricultura - Brasil
[2] Universidade de São Paulo. Centro de Energia Nuclear na Agricultura - Brasil
[3] Universidade de São Paulo. Centro de Energia Nuclear na Agricultura - Brasil
[4] Universidade de São Paulo. Centro de Energia Nuclear na Agricultura - Brasil
[5] Universidade de São Paulo. Centro de Energia Nuclear na Agricultura - Brasil
[6] Universidade de São Paulo. Escola Superior de Agricultura Luiz de Queiroz. Departament of Rural Engineering - Brasil
Total Affiliations: 6
Document type: Journal article
Source: Brazilian Journal of Physics; v. 34, p. 728-731, 2004-09-00.
Abstract

Compaction processes can influence soil physical properties such as soil density, porosity, pore size distribution, and processes like soil water and nutrient movements, root system distribution, and others. Soil porosity modification has important consequences like alterations in results of soil water retention curves. These alterations may cause differences in soil water storage calculations and matric potential values, which are utilized in irrigation management systems. Because of this, soil-sampling techniques should avoid alterations of sample structure. In this work soil sample compaction caused by core sampling devices was investigated using the gamma ray computed tomography technique. A first generation tomograph with fixed source-detector arrangement and translation/rotational movements of the sample was utilized to obtain the images. The radioactive source is 241Am, with an activity of 3.7 GBq, and the detector consists of a 3 in. x 3in. NaI(Tl) scintillation crystal coupled to a photomultiplier tube. Soil samples were taken from an experimental field utilizing cylinders 4.0 cm high and 2.6 cm in diameter. Based on image analyses it was possible to detect compacted regions in all samples next to the cylinder wall due to the sampling system. Tomographic unit profiles of the sample permitted to identify higher values of soil density for deeper regions of the sample, and it was possible to determine the average densities and thickness of these layers. Tomographic analyses showed to be a very useful tool for soil compaction characterization and presented many advantages in relation to traditional methods. (AU)