THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY

Analysis of the soil pore system represents an important way of characterizing soil structure. Properties such as the shape and number of pores can be determined through soil pore evaluations. This study presents a three-dimensional (3D) characterization of the shape and number of pores of a sub-tro...

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Main Authors: Sabrina Passoni, Luiz Fernando Pires, Richard Heck, Jadir Aparecido Rosa
Format: Article
Language:English
Published: Sociedade Brasileira de Ciência do Solo 2015-04-01
Series:Revista Brasileira de Ciência do Solo
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832015000200448&lng=en&tlng=en
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spelling doaj-35622784f6c34ad8b684c923f00bb8d92021-01-02T06:35:02ZengSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo1806-96572015-04-0139244845710.1590/01000683rbcs20140360S0100-06832015000200448THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHYSabrina PassoniLuiz Fernando PiresRichard HeckJadir Aparecido RosaAnalysis of the soil pore system represents an important way of characterizing soil structure. Properties such as the shape and number of pores can be determined through soil pore evaluations. This study presents a three-dimensional (3D) characterization of the shape and number of pores of a sub-tropical soil. To do so, a second generation X-ray microtomograph equipped with a plain type detector was employed. A voltage of 120 kV and current of 80 mA was applied to the X-ray tube. The soil samples analyzed were collected at three different depths (0-10, 10-20, and 20-30 cm). The results obtained allowed qualitative (images) and quantitative (3D) analyses of the soil structure, revealing the potential of the microtomographic technique, as well as the study of differences in soil macroporosity at different depths. Macroporosity was 5.14 % in the 0-10 cm layer, 5.10 % in the 10-20 cm layer, and 6.64 % in the 20-30 cm layer. The macroporosity of unclassified pores (UN) was 0.30 % (0-10 and 10-20 cm) and 0.40 % (20-30 cm), while equant pores (EQ) had values of 0.01 % at the three depths under analysis.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832015000200448&lng=en&tlng=enestrutura do solodistribuição do tamanho de porosporosidade do soloanálise de imagenscomponentes microestruturais do solo
collection DOAJ
language English
format Article
sources DOAJ
author Sabrina Passoni
Luiz Fernando Pires
Richard Heck
Jadir Aparecido Rosa
spellingShingle Sabrina Passoni
Luiz Fernando Pires
Richard Heck
Jadir Aparecido Rosa
THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
Revista Brasileira de Ciência do Solo
estrutura do solo
distribuição do tamanho de poros
porosidade do solo
análise de imagens
componentes microestruturais do solo
author_facet Sabrina Passoni
Luiz Fernando Pires
Richard Heck
Jadir Aparecido Rosa
author_sort Sabrina Passoni
title THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
title_short THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
title_full THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
title_fullStr THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
title_full_unstemmed THREE DIMENSIONAL CHARACTERIZATION OF SOIL MACROPOROSITY BY X-RAY MICROTOMOGRAPHY
title_sort three dimensional characterization of soil macroporosity by x-ray microtomography
publisher Sociedade Brasileira de Ciência do Solo
series Revista Brasileira de Ciência do Solo
issn 1806-9657
publishDate 2015-04-01
description Analysis of the soil pore system represents an important way of characterizing soil structure. Properties such as the shape and number of pores can be determined through soil pore evaluations. This study presents a three-dimensional (3D) characterization of the shape and number of pores of a sub-tropical soil. To do so, a second generation X-ray microtomograph equipped with a plain type detector was employed. A voltage of 120 kV and current of 80 mA was applied to the X-ray tube. The soil samples analyzed were collected at three different depths (0-10, 10-20, and 20-30 cm). The results obtained allowed qualitative (images) and quantitative (3D) analyses of the soil structure, revealing the potential of the microtomographic technique, as well as the study of differences in soil macroporosity at different depths. Macroporosity was 5.14 % in the 0-10 cm layer, 5.10 % in the 10-20 cm layer, and 6.64 % in the 20-30 cm layer. The macroporosity of unclassified pores (UN) was 0.30 % (0-10 and 10-20 cm) and 0.40 % (20-30 cm), while equant pores (EQ) had values of 0.01 % at the three depths under analysis.
topic estrutura do solo
distribuição do tamanho de poros
porosidade do solo
análise de imagens
componentes microestruturais do solo
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832015000200448&lng=en&tlng=en
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AT luizfernandopires threedimensionalcharacterizationofsoilmacroporositybyxraymicrotomography
AT richardheck threedimensionalcharacterizationofsoilmacroporositybyxraymicrotomography
AT jadiraparecidorosa threedimensionalcharacterizationofsoilmacroporositybyxraymicrotomography
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