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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Main Authors: Khoshini Mohammad, Khoshghalb Arman, Khalili Nasser
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/18/e3sconf_isg2019_09002.pdf
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spelling 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
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