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Influence of End Restraints on Strain Responses of Anisotropic Tuff During Triaxial Compression
In triaxial tests, the rock specimen is often assumed to have an axisymmetric elementary response. However, the axisymmetric condition of deformation is not always satisfied for anisotropic rocks, because the incremental relationships between stresses and strains are not necessarily coaxial. Further...
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Published in: | Rock mechanics and rock engineering 2022-06, Vol.55 (6), p.3367-3384 |
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creator | Togashi, Yota Kikumoto, Mamoru Tani, Kazuo Hosoda, Koichi Ogawa, Koji |
description | In triaxial tests, the rock specimen is often assumed to have an axisymmetric elementary response. However, the axisymmetric condition of deformation is not always satisfied for anisotropic rocks, because the incremental relationships between stresses and strains are not necessarily coaxial. Furthermore, rock specimens often exhibit non-uniform deformation owing to the effect of end restraints. The influence of end restraints on the deformation behavior is significant in anisotropic rocks when compared with that in isotropic rocks. In this study, four types of consolidated drained triaxial tests were conducted on anisotropic tuff under different conditions involving end restraints. All components of the strain tensor were measured using multiple strain gauges attached to the side of the specimen. Although the normal strains were not considerably influenced by the presence or absence of the cap and Teflon sheets at the top end of the specimens, the shear strains and orientations of the principal strains were significantly influenced by the end restraints. These results indicate that anisotropic elastic parameters determined using shear strains vary widely owing to end restraints.
Highlights
Triaxial tests were conducted on anisotropic tuff under four end restraint conditions.
Normal strains are not dependent on end restraints.
Shear strains show quite different trends in each case.
Influence of end restraints on anisotropic elastic properties are significantly large.
Low frictional end condition is quite important to detect anisotropic elastic parameters precisely. |
doi_str_mv | 10.1007/s00603-022-02793-z |
format | article |
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Highlights
Triaxial tests were conducted on anisotropic tuff under four end restraint conditions.
Normal strains are not dependent on end restraints.
Shear strains show quite different trends in each case.
Influence of end restraints on anisotropic elastic properties are significantly large.
Low frictional end condition is quite important to detect anisotropic elastic parameters precisely.</description><identifier>ISSN: 0723-2632</identifier><identifier>EISSN: 1434-453X</identifier><identifier>DOI: 10.1007/s00603-022-02793-z</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Anisotropic rocks ; Anisotropy ; Axial strain ; Civil Engineering ; Compression ; Constraints ; Deformation ; Deformation effects ; Earth and Environmental Science ; Earth Sciences ; Elastic anisotropy ; Elastic properties ; Gauges ; Geophysics/Geodesy ; Original Paper ; Parameters ; Polytetrafluoroethylene ; Rocks ; Shear ; Shear strain ; Strain gauges ; Tensors ; Tests ; Triaxial tests ; Tuff</subject><ispartof>Rock mechanics and rock engineering, 2022-06, Vol.55 (6), p.3367-3384</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2022</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c385t-b3eb7bf173a11776f185cdfd9167e393e629d155a8ab5c546231d70d3810a3453</citedby><cites>FETCH-LOGICAL-c385t-b3eb7bf173a11776f185cdfd9167e393e629d155a8ab5c546231d70d3810a3453</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Togashi, Yota</creatorcontrib><creatorcontrib>Kikumoto, Mamoru</creatorcontrib><creatorcontrib>Tani, Kazuo</creatorcontrib><creatorcontrib>Hosoda, Koichi</creatorcontrib><creatorcontrib>Ogawa, Koji</creatorcontrib><title>Influence of End Restraints on Strain Responses of Anisotropic Tuff During Triaxial Compression</title><title>Rock mechanics and rock engineering</title><addtitle>Rock Mech Rock Eng</addtitle><description>In triaxial tests, the rock specimen is often assumed to have an axisymmetric elementary response. However, the axisymmetric condition of deformation is not always satisfied for anisotropic rocks, because the incremental relationships between stresses and strains are not necessarily coaxial. Furthermore, rock specimens often exhibit non-uniform deformation owing to the effect of end restraints. The influence of end restraints on the deformation behavior is significant in anisotropic rocks when compared with that in isotropic rocks. In this study, four types of consolidated drained triaxial tests were conducted on anisotropic tuff under different conditions involving end restraints. All components of the strain tensor were measured using multiple strain gauges attached to the side of the specimen. Although the normal strains were not considerably influenced by the presence or absence of the cap and Teflon sheets at the top end of the specimens, the shear strains and orientations of the principal strains were significantly influenced by the end restraints. These results indicate that anisotropic elastic parameters determined using shear strains vary widely owing to end restraints.
Highlights
Triaxial tests were conducted on anisotropic tuff under four end restraint conditions.
Normal strains are not dependent on end restraints.
Shear strains show quite different trends in each case.
Influence of end restraints on anisotropic elastic properties are significantly large.
Low frictional end condition is quite important to detect anisotropic elastic parameters precisely.</description><subject>Anisotropic rocks</subject><subject>Anisotropy</subject><subject>Axial strain</subject><subject>Civil Engineering</subject><subject>Compression</subject><subject>Constraints</subject><subject>Deformation</subject><subject>Deformation effects</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Elastic anisotropy</subject><subject>Elastic properties</subject><subject>Gauges</subject><subject>Geophysics/Geodesy</subject><subject>Original Paper</subject><subject>Parameters</subject><subject>Polytetrafluoroethylene</subject><subject>Rocks</subject><subject>Shear</subject><subject>Shear strain</subject><subject>Strain gauges</subject><subject>Tensors</subject><subject>Tests</subject><subject>Triaxial tests</subject><subject>Tuff</subject><issn>0723-2632</issn><issn>1434-453X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp9UE1LxDAQDaLguvoHPAU8V_PRJO1xWVddWBC0greQtolk2U1q0oLurzfdCt48DDPMvPeG9wC4xugWIyTuIkIc0QwRkkqUNDucgBnOaZ7ljL6fghkShGaEU3IOLmLcIpSOopgBuXZmN2jXaOgNXLkWvujYB2VdH6F38PU4j8vOu6jjiFo4G30ffGcbWA3GwPshWPcBq2DVl1U7uPT7LugYrXeX4MyoXdRXv30O3h5W1fIp2zw_rpeLTdbQgvVZTXUtaoMFVRgLwQ0uWNOatsRcaFpSzUnZYsZUoWrWsJwTiluBWlpgpGjyOAc3k24X_OeQLMitH4JLLyXhImdcJNWEIhOqCT7GoI3sgt2r8C0xkmOQcgpSpiDlMUh5SCQ6kWI32tThT_of1g9LZnbL</recordid><startdate>20220601</startdate><enddate>20220601</enddate><creator>Togashi, Yota</creator><creator>Kikumoto, Mamoru</creator><creator>Tani, Kazuo</creator><creator>Hosoda, Koichi</creator><creator>Ogawa, Koji</creator><general>Springer Vienna</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20220601</creationdate><title>Influence of End Restraints on Strain Responses of Anisotropic Tuff During Triaxial Compression</title><author>Togashi, Yota ; Kikumoto, Mamoru ; Tani, Kazuo ; Hosoda, Koichi ; Ogawa, Koji</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-b3eb7bf173a11776f185cdfd9167e393e629d155a8ab5c546231d70d3810a3453</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Anisotropic rocks</topic><topic>Anisotropy</topic><topic>Axial strain</topic><topic>Civil Engineering</topic><topic>Compression</topic><topic>Constraints</topic><topic>Deformation</topic><topic>Deformation effects</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Elastic anisotropy</topic><topic>Elastic properties</topic><topic>Gauges</topic><topic>Geophysics/Geodesy</topic><topic>Original Paper</topic><topic>Parameters</topic><topic>Polytetrafluoroethylene</topic><topic>Rocks</topic><topic>Shear</topic><topic>Shear strain</topic><topic>Strain gauges</topic><topic>Tensors</topic><topic>Tests</topic><topic>Triaxial tests</topic><topic>Tuff</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Togashi, Yota</creatorcontrib><creatorcontrib>Kikumoto, Mamoru</creatorcontrib><creatorcontrib>Tani, Kazuo</creatorcontrib><creatorcontrib>Hosoda, Koichi</creatorcontrib><creatorcontrib>Ogawa, Koji</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Science Journals</collection><collection>Engineering Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering collection</collection><collection>ProQuest Central Basic</collection><jtitle>Rock mechanics and rock engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Togashi, Yota</au><au>Kikumoto, Mamoru</au><au>Tani, Kazuo</au><au>Hosoda, Koichi</au><au>Ogawa, Koji</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of End Restraints on Strain Responses of Anisotropic Tuff During Triaxial Compression</atitle><jtitle>Rock mechanics and rock engineering</jtitle><stitle>Rock Mech Rock Eng</stitle><date>2022-06-01</date><risdate>2022</risdate><volume>55</volume><issue>6</issue><spage>3367</spage><epage>3384</epage><pages>3367-3384</pages><issn>0723-2632</issn><eissn>1434-453X</eissn><abstract>In triaxial tests, the rock specimen is often assumed to have an axisymmetric elementary response. However, the axisymmetric condition of deformation is not always satisfied for anisotropic rocks, because the incremental relationships between stresses and strains are not necessarily coaxial. Furthermore, rock specimens often exhibit non-uniform deformation owing to the effect of end restraints. The influence of end restraints on the deformation behavior is significant in anisotropic rocks when compared with that in isotropic rocks. In this study, four types of consolidated drained triaxial tests were conducted on anisotropic tuff under different conditions involving end restraints. All components of the strain tensor were measured using multiple strain gauges attached to the side of the specimen. Although the normal strains were not considerably influenced by the presence or absence of the cap and Teflon sheets at the top end of the specimens, the shear strains and orientations of the principal strains were significantly influenced by the end restraints. These results indicate that anisotropic elastic parameters determined using shear strains vary widely owing to end restraints.
Highlights
Triaxial tests were conducted on anisotropic tuff under four end restraint conditions.
Normal strains are not dependent on end restraints.
Shear strains show quite different trends in each case.
Influence of end restraints on anisotropic elastic properties are significantly large.
Low frictional end condition is quite important to detect anisotropic elastic parameters precisely.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00603-022-02793-z</doi><tpages>18</tpages></addata></record> |
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subjects | Anisotropic rocks Anisotropy Axial strain Civil Engineering Compression Constraints Deformation Deformation effects Earth and Environmental Science Earth Sciences Elastic anisotropy Elastic properties Gauges Geophysics/Geodesy Original Paper Parameters Polytetrafluoroethylene Rocks Shear Shear strain Strain gauges Tensors Tests Triaxial tests Tuff |
title | Influence of End Restraints on Strain Responses of Anisotropic Tuff During Triaxial Compression |
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