Compressive behaviour of very dense structured granular geo-materials
The isotropic compression behaviour of dense structured geo-materials and the associated degradation at failure is addressed in a non-qualitative manner. To this end, the general behaviour of fully de-structured geo-materials, e.g. sands, as an accepted reference is thoroughly investigated. The para...
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EDP Sciences
2019-01-01
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doaj-8d207db2018e49559bcfc416839849682021-02-02T05:32:35ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01920900210.1051/e3sconf/20199209002e3sconf_isg2019_09002Compressive behaviour of very dense structured granular geo-materialsKhoshini MohammadKhoshghalb ArmanKhalili NasserThe isotropic compression behaviour of dense structured geo-materials and the associated degradation at failure is addressed in a non-qualitative manner. To this end, the general behaviour of fully de-structured geo-materials, e.g. sands, as an accepted reference is thoroughly investigated. The parameters affecting the behaviour of de-structured materials such as mineralogy, gradation and fines content, and relative density are discussed. The isotropic compression behaviour of a weathered weak sandstone, representative of a structured granular geo-material, is then investigated along the isotropic compression stress path under a range of pressures from nil to 100 MPa. Both structured and fully de-structured states of the material are tested implementing the proposed quantification method. The effect of structure on the compressibility of the material is found to be tangible. By plotting the specific volume versus natural log of the mean effective stress, the onset of structure collapse and the successive degradation of the structure are captured. By increasing the pressure, compaction bands throughout the sample increasingly develop and the compression curve asymptotically approaches to that of the fully degraded state of the material. At elevated pressures, the rate of compressibility will increase significantly due to particle crushing.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/18/e3sconf_isg2019_09002.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Khoshini Mohammad Khoshghalb Arman Khalili Nasser |
spellingShingle |
Khoshini Mohammad Khoshghalb Arman Khalili Nasser Compressive behaviour of very dense structured granular geo-materials E3S Web of Conferences |
author_facet |
Khoshini Mohammad Khoshghalb Arman Khalili Nasser |
author_sort |
Khoshini Mohammad |
title |
Compressive behaviour of very dense structured granular geo-materials |
title_short |
Compressive behaviour of very dense structured granular geo-materials |
title_full |
Compressive behaviour of very dense structured granular geo-materials |
title_fullStr |
Compressive behaviour of very dense structured granular geo-materials |
title_full_unstemmed |
Compressive behaviour of very dense structured granular geo-materials |
title_sort |
compressive behaviour of very dense structured granular geo-materials |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2019-01-01 |
description |
The isotropic compression behaviour of dense structured geo-materials and the associated degradation at failure is addressed in a non-qualitative manner. To this end, the general behaviour of fully de-structured geo-materials, e.g. sands, as an accepted reference is thoroughly investigated. The parameters affecting the behaviour of de-structured materials such as mineralogy, gradation and fines content, and relative density are discussed. The isotropic compression behaviour of a weathered weak sandstone, representative of a structured granular geo-material, is then investigated along the isotropic compression stress path under a range of pressures from nil to 100 MPa. Both structured and fully de-structured states of the material are tested implementing the proposed quantification method. The effect of structure on the compressibility of the material is found to be tangible. By plotting the specific volume versus natural log of the mean effective stress, the onset of structure collapse and the successive degradation of the structure are captured. By increasing the pressure, compaction bands throughout the sample increasingly develop and the compression curve asymptotically approaches to that of the fully degraded state of the material. At elevated pressures, the rate of compressibility will increase significantly due to particle crushing. |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/18/e3sconf_isg2019_09002.pdf |
work_keys_str_mv |
AT khoshinimohammad compressivebehaviourofverydensestructuredgranulargeomaterials AT khoshghalbarman compressivebehaviourofverydensestructuredgranulargeomaterials AT khalilinasser compressivebehaviourofverydensestructuredgranulargeomaterials |
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1724303490466971648 |