Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction

Currently in Brazil, as in other parts of the world, the concern is great with the increase of degraded agricultural soil, which is mostly related to the occurrence of soil compaction. Although soil texture is recognized as a very important component in the soil compressive behaviors, there are few...

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Main Authors: Eduardo da Costa Severiano, Geraldo César de Oliveira, Moacir de Souza Dias Júnior, Katia Aparecida de Pinho Costa, Vinícius de Melo Benites, Silvio Marcos Ferreira Filho
Format: Article
Language:English
Published: Sociedade Brasileira de Ciência do Solo 2011-06-01
Series:Revista Brasileira de Ciência do Solo
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300014&lng=en&tlng=en
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spelling doaj-689472b2fa2a491f93752571049b96322021-01-02T08:09:23ZengSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo1806-96572011-06-0135378379110.1590/S0100-06832011000300014S0100-06832011000300014Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compactionEduardo da Costa Severiano0Geraldo César de Oliveira1Moacir de Souza Dias Júnior2Katia Aparecida de Pinho Costa3Vinícius de Melo Benites4Silvio Marcos Ferreira Filho5Instituto Federal GoianoUniversidade Federal de LavrasUniversidade Federal de LavrasInstituto Federal GoianoEmbrapaUniversidade de Rio VerdeCurrently in Brazil, as in other parts of the world, the concern is great with the increase of degraded agricultural soil, which is mostly related to the occurrence of soil compaction. Although soil texture is recognized as a very important component in the soil compressive behaviors, there are few studies that quantify its influence on the structural changes of Latosols in the Brazilian Cerrado region. This study aimed to evaluate structural changes and the compressive behavior of Latosols in Rio Verde, Goiás, through the modeling of additional soil compaction. The study was carried out using five Latosols with very different textures, under different soil compaction levels. Water retention and soil compression curves, and bearing capacity models were determined from undisturbed samples collected on the B horizons. Results indicated that clayey and very clayey Latosols were more susceptible to compression than medium-textured soils. Soil compression curves at density values associate with edaphic functions were used to determine the beneficial pressure (σ b) , i.e., pressure with optimal water retention, and critical pressure (σcrMAC), i.e., pressure with macroporosity below critical levels. These pressure values were higher than the preconsolidation pressure (σp), and therefore characterized as additional compaction. Based on the compressive behavior of these Latosols, it can be concluded that the combined preconsolidation pressure, beneficial pressure and critical pressure allow a better understanding of compression processes of Latosols.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300014&lng=en&tlng=enpressão de preconsolidaçãopressão benéficapressão críticadegradação do solodistribuição de partículas por tamanho
collection DOAJ
language English
format Article
sources DOAJ
author Eduardo da Costa Severiano
Geraldo César de Oliveira
Moacir de Souza Dias Júnior
Katia Aparecida de Pinho Costa
Vinícius de Melo Benites
Silvio Marcos Ferreira Filho
spellingShingle Eduardo da Costa Severiano
Geraldo César de Oliveira
Moacir de Souza Dias Júnior
Katia Aparecida de Pinho Costa
Vinícius de Melo Benites
Silvio Marcos Ferreira Filho
Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
Revista Brasileira de Ciência do Solo
pressão de preconsolidação
pressão benéfica
pressão crítica
degradação do solo
distribuição de partículas por tamanho
author_facet Eduardo da Costa Severiano
Geraldo César de Oliveira
Moacir de Souza Dias Júnior
Katia Aparecida de Pinho Costa
Vinícius de Melo Benites
Silvio Marcos Ferreira Filho
author_sort Eduardo da Costa Severiano
title Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
title_short Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
title_full Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
title_fullStr Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
title_full_unstemmed Structural changes in latosols of the cerrado region: II - soil compressive behavior and modeling of additional compaction
title_sort structural changes in latosols of the cerrado region: ii - soil compressive behavior and modeling of additional compaction
publisher Sociedade Brasileira de Ciência do Solo
series Revista Brasileira de Ciência do Solo
issn 1806-9657
publishDate 2011-06-01
description Currently in Brazil, as in other parts of the world, the concern is great with the increase of degraded agricultural soil, which is mostly related to the occurrence of soil compaction. Although soil texture is recognized as a very important component in the soil compressive behaviors, there are few studies that quantify its influence on the structural changes of Latosols in the Brazilian Cerrado region. This study aimed to evaluate structural changes and the compressive behavior of Latosols in Rio Verde, Goiás, through the modeling of additional soil compaction. The study was carried out using five Latosols with very different textures, under different soil compaction levels. Water retention and soil compression curves, and bearing capacity models were determined from undisturbed samples collected on the B horizons. Results indicated that clayey and very clayey Latosols were more susceptible to compression than medium-textured soils. Soil compression curves at density values associate with edaphic functions were used to determine the beneficial pressure (σ b) , i.e., pressure with optimal water retention, and critical pressure (σcrMAC), i.e., pressure with macroporosity below critical levels. These pressure values were higher than the preconsolidation pressure (σp), and therefore characterized as additional compaction. Based on the compressive behavior of these Latosols, it can be concluded that the combined preconsolidation pressure, beneficial pressure and critical pressure allow a better understanding of compression processes of Latosols.
topic pressão de preconsolidação
pressão benéfica
pressão crítica
degradação do solo
distribuição de partículas por tamanho
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000300014&lng=en&tlng=en
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