Experimental Study Effect of the Shaliness on Physical Properties of Soil
Autor(a) principal: | |
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Data de Publicação: | 2016 |
Outros Autores: | , |
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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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 info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
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) |
instacron_str |
UFRJ |
institution |
UFRJ |
reponame_str |
Anuário do Instituto de Geociências (Online) |
collection |
Anuário do Instituto de Geociências (Online) |
repository.name.fl_str_mv |
Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ) |
repository.mail.fl_str_mv |
anuario@igeo.ufrj.br|| |
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1797053536776749056 |