Experimental Study Effect of the Shaliness on Physical Properties of Soil

Detalhes bibliográficos
Autor(a) principal: Carvalho, Maura Renata de Toledo
Data de Publicação: 2016
Outros Autores: Dias, Gleide Alencar do Nascimento, Soares, José Agnelo
Tipo de documento: Artigo
Idioma: por
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/7003
Resumo: This final course work aimed to evaluate the effect of shaliness on the physical properties of clay soils, with emphasis on the properties of porous media. For this, we used a gas poropermeameter based on the pressure variation on confining chamber, in order to obtain values of absolute permeability and effective porosity on unconsolidated sediments (soils). The values for pore volume are obtained by Boyle Mariotte law, which relates the variation of pressure and volume of an ideal gas at constant temperature, while permeability values are obtained by Darcy's law. It is also emphasized the development of a method for analysis of unconsolidated sediments with the equipment since it was designed to consolidated sediments. This includes sample enveloping and studies for determination of ideal pressures and flows to be used. Measured values for permeability and porosity were used in estimating other physical parameter of the sediments, the specific surface of the grains, through the Kozeny-Carman equation, whose constant was considered equal to 5, since this is the value recommended for flow in porous unconsolidated sediments. Results show that this equipment can be used successfully for measurements of physical pore properties of soils if samples are properly prepared.
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spelling Experimental Study Effect of the Shaliness on Physical Properties of SoilEstudo Experimental do Efeito da Argilosidade Sobre as Propriedades Físicas de SolosShaliness; Permeability; Porosity.Argilosidade; Permeabilidade; Porosidade.This final course work aimed to evaluate the effect of shaliness on the physical properties of clay soils, with emphasis on the properties of porous media. For this, we used a gas poropermeameter based on the pressure variation on confining chamber, in order to obtain values of absolute permeability and effective porosity on unconsolidated sediments (soils). The values for pore volume are obtained by Boyle Mariotte law, which relates the variation of pressure and volume of an ideal gas at constant temperature, while permeability values are obtained by Darcy's law. It is also emphasized the development of a method for analysis of unconsolidated sediments with the equipment since it was designed to consolidated sediments. This includes sample enveloping and studies for determination of ideal pressures and flows to be used. Measured values for permeability and porosity were used in estimating other physical parameter of the sediments, the specific surface of the grains, through the Kozeny-Carman equation, whose constant was considered equal to 5, since this is the value recommended for flow in porous unconsolidated sediments. Results show that this equipment can be used successfully for measurements of physical pore properties of soils if samples are properly prepared.Neste trabalho foi avaliado o efeito da argilosidade sobre as propriedades físicas de solos argilosos, com ênfase na porosidade e na permeabilidade do meio. Para isto foi utilizado o equipamento permo-porosímetro a gás, baseado na variação de pressão em câmara confinante, com o intuito de obter valores de porosidade efetiva e permeabilidade absoluta em sedimentos inconsolidados (solos). No procedimento foram utilizadas amostras sintéticas, usando diferentes proporções de quantidades de esferas de vidro e caulinita (argila), com a intenção de criar um padrão granulométrico das amostras a serem analisadas. Isto incluiu a preparação do invólucro da amostra e estudos da determinação das pressões e fluxos de fluidos a serem aplicados nas amostras, fundamentados em publicações científicas. Os valores obtidos de permeabilidade e porosidade foram utilizados na estimativa de outro parâmetro físico dos sedimentos, a superfície específica dos grãos através da equação de Kozeny-Carman, cujo valor da constante recomendado por outros autores é igual a 5, para fluxo em meios porosos inconsolidados. Pode-se verificar nos resultados que o permo-porosímetro a gás, pode ser utilizado com sucesso na medição das propriedades físicas de solos tanto arenosos como argilosos.Universidade Federal do Rio de Janeiro2016-06-23info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/700310.11137/2016_2_108_115Anuário do Instituto de Geociências; Vol 39, No 2 (2016); 108-115Anuário do Instituto de Geociências; Vol 39, No 2 (2016); 108-1151982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/7003/5570Copyright (c) 2016 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessCarvalho, Maura Renata de ToledoDias, Gleide Alencar do NascimentoSoares, José Agnelo2017-01-23T22:48:34Zoai:www.revistas.ufrj.br:article/7003Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-01-23T22:48:34Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Experimental Study Effect of the Shaliness on Physical Properties of Soil
Estudo Experimental do Efeito da Argilosidade Sobre as Propriedades Físicas de Solos
title Experimental Study Effect of the Shaliness on Physical Properties of Soil
spellingShingle Experimental Study Effect of the Shaliness on Physical Properties of Soil
Carvalho, Maura Renata de Toledo
Shaliness; Permeability; Porosity.
Argilosidade; Permeabilidade; Porosidade.
title_short Experimental Study Effect of the Shaliness on Physical Properties of Soil
title_full Experimental Study Effect of the Shaliness on Physical Properties of Soil
title_fullStr Experimental Study Effect of the Shaliness on Physical Properties of Soil
title_full_unstemmed Experimental Study Effect of the Shaliness on Physical Properties of Soil
title_sort Experimental Study Effect of the Shaliness on Physical Properties of Soil
author Carvalho, Maura Renata de Toledo
author_facet Carvalho, Maura Renata de Toledo
Dias, Gleide Alencar do Nascimento
Soares, José Agnelo
author_role author
author2 Dias, Gleide Alencar do Nascimento
Soares, José Agnelo
author2_role author
author
dc.contributor.author.fl_str_mv Carvalho, Maura Renata de Toledo
Dias, Gleide Alencar do Nascimento
Soares, José Agnelo
dc.subject.por.fl_str_mv Shaliness; Permeability; Porosity.
Argilosidade; Permeabilidade; Porosidade.
topic Shaliness; Permeability; Porosity.
Argilosidade; Permeabilidade; Porosidade.
description This final course work aimed to evaluate the effect of shaliness on the physical properties of clay soils, with emphasis on the properties of porous media. For this, we used a gas poropermeameter based on the pressure variation on confining chamber, in order to obtain values of absolute permeability and effective porosity on unconsolidated sediments (soils). The values for pore volume are obtained by Boyle Mariotte law, which relates the variation of pressure and volume of an ideal gas at constant temperature, while permeability values are obtained by Darcy's law. It is also emphasized the development of a method for analysis of unconsolidated sediments with the equipment since it was designed to consolidated sediments. This includes sample enveloping and studies for determination of ideal pressures and flows to be used. Measured values for permeability and porosity were used in estimating other physical parameter of the sediments, the specific surface of the grains, through the Kozeny-Carman equation, whose constant was considered equal to 5, since this is the value recommended for flow in porous unconsolidated sediments. Results show that this equipment can be used successfully for measurements of physical pore properties of soils if samples are properly prepared.
publishDate 2016
dc.date.none.fl_str_mv 2016-06-23
dc.type.none.fl_str_mv
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/7003
10.11137/2016_2_108_115
url https://revistas.ufrj.br/index.php/aigeo/article/view/7003
identifier_str_mv 10.11137/2016_2_108_115
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/7003/5570
dc.rights.driver.fl_str_mv Copyright (c) 2016 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2016 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 39, No 2 (2016); 108-115
Anuário do Instituto de Geociências; Vol 39, No 2 (2016); 108-115
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
instname_str Universidade Federal do Rio de Janeiro (UFRJ)
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reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
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