Deformation and hysteresis behaviors of sandstone exposed to distinct sequences of variable-frequency compressive cyclic stresses
The response of rock to dynamic loading is critical to the stability of underground engineering. This study experimentally investigated the mechanical responses of sandstone exposed to incremental and decremental frequency under compressive cyclic loading. The impact of loading frequency on amplitud...
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description | The response of rock to dynamic loading is critical to the stability of underground engineering. This study experimentally investigated the mechanical responses of sandstone exposed to incremental and decremental frequency under compressive cyclic loading. The impact of loading frequency on amplitude of strain variation between the upper and lower bounds of cyclic stresses are revealed. The result shows that a higher frequency can incur a larger-amplitude variation of axial and volumetric strains between two bounds of cyclic stresses. The inelastic axial and radial strain ratios (defined in text) both exhibit good performance in early warning of rock failure. The cyclic loading stage (CLS) with the lowest inelastic strain ratio can be defined as the critical phase. This also applies to the evolution of secant modulus, the CLS with the peak secant modulus is used as the point to emit warning signals. The phase shift between stress–strain is frequency-dependent, a lower frequency results in a larger phase-shift. The evolution of damping ratio and dissipated energy ratio are almost frequency independent and both decrease with the ongoing of cycle. |
doi_str_mv | 10.1007/s12665-023-11327-x |
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This also applies to the evolution of secant modulus, the CLS with the peak secant modulus is used as the point to emit warning signals. The phase shift between stress–strain is frequency-dependent, a lower frequency results in a larger phase-shift. The evolution of damping ratio and dissipated energy ratio are almost frequency independent and both decrease with the ongoing of cycle.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-023-11327-x</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Amplitude ; Amplitudes ; Axial stress ; Biogeosciences ; Civil engineering ; Coal mining ; Compressive properties ; Cyclic loading ; Cyclic loads ; Damping ; Damping ratio ; Deformation ; Dynamic loads ; Dynamic stability ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Energy dissipation ; Environmental Science and Engineering ; Evolution ; Frequency dependence ; Geochemistry ; Geology ; Heat treating ; Hydrology/Water Resources ; Investigations ; Load ; Lower bounds ; Mechanical loading ; Original Article ; Phase shift ; Rocks ; Sandstone ; Sedimentary rocks ; Strain ; Stress ; Terrestrial Pollution</subject><ispartof>Environmental earth sciences, 2024-03, Vol.83 (5), p.150, Article 150</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a293t-23f53121dc3fe6f803c0b68a30c73a994c3cbdc509c61f2a3da936afbf9ec4da3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-023-11327-x$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-023-11327-x$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Song, Z. 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The result shows that a higher frequency can incur a larger-amplitude variation of axial and volumetric strains between two bounds of cyclic stresses. The inelastic axial and radial strain ratios (defined in text) both exhibit good performance in early warning of rock failure. The cyclic loading stage (CLS) with the lowest inelastic strain ratio can be defined as the critical phase. This also applies to the evolution of secant modulus, the CLS with the peak secant modulus is used as the point to emit warning signals. The phase shift between stress–strain is frequency-dependent, a lower frequency results in a larger phase-shift. The evolution of damping ratio and dissipated energy ratio are almost frequency independent and both decrease with the ongoing of cycle.</description><subject>Amplitude</subject><subject>Amplitudes</subject><subject>Axial stress</subject><subject>Biogeosciences</subject><subject>Civil engineering</subject><subject>Coal mining</subject><subject>Compressive properties</subject><subject>Cyclic loading</subject><subject>Cyclic loads</subject><subject>Damping</subject><subject>Damping ratio</subject><subject>Deformation</subject><subject>Dynamic loads</subject><subject>Dynamic stability</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Energy dissipation</subject><subject>Environmental Science and Engineering</subject><subject>Evolution</subject><subject>Frequency dependence</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Heat treating</subject><subject>Hydrology/Water Resources</subject><subject>Investigations</subject><subject>Load</subject><subject>Lower bounds</subject><subject>Mechanical loading</subject><subject>Original Article</subject><subject>Phase shift</subject><subject>Rocks</subject><subject>Sandstone</subject><subject>Sedimentary rocks</subject><subject>Strain</subject><subject>Stress</subject><subject>Terrestrial Pollution</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9UEtLAzEQXkTBUvsHPAU8ryaZNm2O4hsKXvQcstmJTWk3NRNLe_SfG7uiN-cyw8z3GL6qOhf8UnA-vSIhlZrUXEItBMhpvTuqBmKmVK2k1se_84yfViOiJS8FAjRXg-rzFn1Ma5tD7JjtWrbYU8aEFIg1uLDbEBOx6BmVI-XYIcPdJhK2LEfWBsqhc5kRvn9g5_AA3doUbLPC2qd-vWcurjdFlMIWmdu7VXCM8vcC6aw68XZFOPrpw-r1_u7l5rGePz883VzPays15FqCn4CQonXgUfkZB8cbNbPA3RSs1mMHrmndhGunhJcWWqtBWd94jW7cWhhWF73uJsXyFWWzjB-pK5amGABMOfBxQcke5VIkSujNJoW1TXsjuPlO2_Rpm5K2OaRtdoUEPYkKuHvD9Cf9D-sLDrWHUg</recordid><startdate>20240301</startdate><enddate>20240301</enddate><creator>Song, Z. 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H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a293t-23f53121dc3fe6f803c0b68a30c73a994c3cbdc509c61f2a3da936afbf9ec4da3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Amplitude</topic><topic>Amplitudes</topic><topic>Axial stress</topic><topic>Biogeosciences</topic><topic>Civil engineering</topic><topic>Coal mining</topic><topic>Compressive properties</topic><topic>Cyclic loading</topic><topic>Cyclic loads</topic><topic>Damping</topic><topic>Damping ratio</topic><topic>Deformation</topic><topic>Dynamic loads</topic><topic>Dynamic stability</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Energy dissipation</topic><topic>Environmental Science and Engineering</topic><topic>Evolution</topic><topic>Frequency dependence</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Heat treating</topic><topic>Hydrology/Water Resources</topic><topic>Investigations</topic><topic>Load</topic><topic>Lower bounds</topic><topic>Mechanical loading</topic><topic>Original Article</topic><topic>Phase shift</topic><topic>Rocks</topic><topic>Sandstone</topic><topic>Sedimentary rocks</topic><topic>Strain</topic><topic>Stress</topic><topic>Terrestrial Pollution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Song, Z. 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H.</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Song, Z. Y.</au><au>Zhang, T.</au><au>Dang, W. G.</au><au>Wang, C. P.</au><au>Yang, Z.</au><au>Yu, Z. H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Deformation and hysteresis behaviors of sandstone exposed to distinct sequences of variable-frequency compressive cyclic stresses</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2024-03-01</date><risdate>2024</risdate><volume>83</volume><issue>5</issue><spage>150</spage><pages>150-</pages><artnum>150</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>The response of rock to dynamic loading is critical to the stability of underground engineering. This study experimentally investigated the mechanical responses of sandstone exposed to incremental and decremental frequency under compressive cyclic loading. The impact of loading frequency on amplitude of strain variation between the upper and lower bounds of cyclic stresses are revealed. The result shows that a higher frequency can incur a larger-amplitude variation of axial and volumetric strains between two bounds of cyclic stresses. The inelastic axial and radial strain ratios (defined in text) both exhibit good performance in early warning of rock failure. The cyclic loading stage (CLS) with the lowest inelastic strain ratio can be defined as the critical phase. This also applies to the evolution of secant modulus, the CLS with the peak secant modulus is used as the point to emit warning signals. The phase shift between stress–strain is frequency-dependent, a lower frequency results in a larger phase-shift. The evolution of damping ratio and dissipated energy ratio are almost frequency independent and both decrease with the ongoing of cycle.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-023-11327-x</doi></addata></record> |
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subjects | Amplitude Amplitudes Axial stress Biogeosciences Civil engineering Coal mining Compressive properties Cyclic loading Cyclic loads Damping Damping ratio Deformation Dynamic loads Dynamic stability Earth and Environmental Science Earth science Earth Sciences Energy dissipation Environmental Science and Engineering Evolution Frequency dependence Geochemistry Geology Heat treating Hydrology/Water Resources Investigations Load Lower bounds Mechanical loading Original Article Phase shift Rocks Sandstone Sedimentary rocks Strain Stress Terrestrial Pollution |
title | Deformation and hysteresis behaviors of sandstone exposed to distinct sequences of variable-frequency compressive cyclic stresses |
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