Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test

Specimens of triaxial tests ordinarily response as element in the axisymmetric condition, and it is theoretically correct assumption. However, for anisotropic rocks, the axisymmetric condition is not always satisfied because incremental relationships between stresses and strains are not coaxial. In...

Full description

Bibliographic Details
Main Authors: Togashi Yota, Kikumoto Mamoru, Tani Kazuo, Hosoda Koichi, Ogawa Koji
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_02008.pdf
id doaj-daac8d30642b45c08e3f4b5c68c708f4
record_format Article
spelling doaj-daac8d30642b45c08e3f4b5c68c708f42021-02-02T02:28:41ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01920200810.1051/e3sconf/20199202008e3sconf_isg2019_02008Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial testTogashi YotaKikumoto MamoruTani KazuoHosoda KoichiOgawa KojiSpecimens of triaxial tests ordinarily response as element in the axisymmetric condition, and it is theoretically correct assumption. However, for anisotropic rocks, the axisymmetric condition is not always satisfied because incremental relationships between stresses and strains are not coaxial. In addition, such rock specimen often shows non-uniform deformation behaviors due to end frictions. As the reason, the influence of end restraints on deformation behaviors of anisotropic rocks during triaxial compression is much greater than that of isotropic one. In this study, the variations in the stress-strain relationships of anisotropic tuff due to the condition of end restraints are investigated. The results of four consolidated drained triaxial tests with measuring the strain tensor demonstrated that the axial and volumetric strains were not influenced by whether sliding mechanism and Teflon sheets are installed at the end of specimens or not; meanwhile, the shear components of the strain tensor and the inclinations of principal strain orientations are widely varied owing to the end restraints.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/18/e3sconf_isg2019_02008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Togashi Yota
Kikumoto Mamoru
Tani Kazuo
Hosoda Koichi
Ogawa Koji
spellingShingle Togashi Yota
Kikumoto Mamoru
Tani Kazuo
Hosoda Koichi
Ogawa Koji
Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
E3S Web of Conferences
author_facet Togashi Yota
Kikumoto Mamoru
Tani Kazuo
Hosoda Koichi
Ogawa Koji
author_sort Togashi Yota
title Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
title_short Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
title_full Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
title_fullStr Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
title_full_unstemmed Non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
title_sort non-axisymmetric and/or non-elementary response of anisotropic tuff in axisymmetric, elementary triaxial test
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2019-01-01
description Specimens of triaxial tests ordinarily response as element in the axisymmetric condition, and it is theoretically correct assumption. However, for anisotropic rocks, the axisymmetric condition is not always satisfied because incremental relationships between stresses and strains are not coaxial. In addition, such rock specimen often shows non-uniform deformation behaviors due to end frictions. As the reason, the influence of end restraints on deformation behaviors of anisotropic rocks during triaxial compression is much greater than that of isotropic one. In this study, the variations in the stress-strain relationships of anisotropic tuff due to the condition of end restraints are investigated. The results of four consolidated drained triaxial tests with measuring the strain tensor demonstrated that the axial and volumetric strains were not influenced by whether sliding mechanism and Teflon sheets are installed at the end of specimens or not; meanwhile, the shear components of the strain tensor and the inclinations of principal strain orientations are widely varied owing to the end restraints.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/18/e3sconf_isg2019_02008.pdf
work_keys_str_mv AT togashiyota nonaxisymmetricandornonelementaryresponseofanisotropictuffinaxisymmetricelementarytriaxialtest
AT kikumotomamoru nonaxisymmetricandornonelementaryresponseofanisotropictuffinaxisymmetricelementarytriaxialtest
AT tanikazuo nonaxisymmetricandornonelementaryresponseofanisotropictuffinaxisymmetricelementarytriaxialtest
AT hosodakoichi nonaxisymmetricandornonelementaryresponseofanisotropictuffinaxisymmetricelementarytriaxialtest
AT ogawakoji nonaxisymmetricandornonelementaryresponseofanisotropictuffinaxisymmetricelementarytriaxialtest
_version_ 1724309786270367744