Dynamic Response and Energy Evolution of Sandstone Under Coupled Static–Dynamic Compression: Insights from Experimental Study into Deep Rock Engineering Applications
To deeply understand the rock failure characteristics under actual engineering condition, in which static geo-stress and dynamic disturbance usually act simultaneously, impact tests were conducted on sandstone subjected to axial static pre-stresses varying from 0 to 75 MPa by a modified split Hopkin...
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description | To deeply understand the rock failure characteristics under actual engineering condition, in which static geo-stress and dynamic disturbance usually act simultaneously, impact tests were conducted on sandstone subjected to axial static pre-stresses varying from 0 to 75 MPa by a modified split Hopkinson pressure bar. The fracturing process of specimens was recorded by a high speed camera. Dynamic parameters of sandstone, such as strain rate, dynamic strength and energy partition were acquired. Fracture mechanisms of pulverized specimens were identified by the method combining the displacement trend line and digital image correlation technique. Moreover, fragments of failed specimens were sieved to obtain the fragment size distribution. Test results revealed that, under the same incident energy, the dynamic compressive strength increases first, then decreases slowly and at last drops rapidly with the increase of pre-stress, and reaches the maximum under 24.4% of uniaxial compressive strength due to the closure of initial defects. Four final patterns were observed, namely intact, axial split, rock burst, and pulverization. The rock burst only occurs when the pre-stress lies in the elastic deformation stage or initial stable crack growth stage and the incident energy is intermediate. For pulverized specimens, the fracture mechanism is transformed into shear/tensile equivalent from tensile-dominated mixed mode as the pre-stress increases. Specimens with 75 MPa pre-stress release strain energy during failure process, contrary to specimens with lower pre-stresses absorbing energy from outside. The crushing degree of pulverized specimens exhibits a positive correlation with the pre-stress as a consequence of higher damage development in rock. |
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The fracturing process of specimens was recorded by a high speed camera. Dynamic parameters of sandstone, such as strain rate, dynamic strength and energy partition were acquired. Fracture mechanisms of pulverized specimens were identified by the method combining the displacement trend line and digital image correlation technique. Moreover, fragments of failed specimens were sieved to obtain the fragment size distribution. Test results revealed that, under the same incident energy, the dynamic compressive strength increases first, then decreases slowly and at last drops rapidly with the increase of pre-stress, and reaches the maximum under 24.4% of uniaxial compressive strength due to the closure of initial defects. Four final patterns were observed, namely intact, axial split, rock burst, and pulverization. The rock burst only occurs when the pre-stress lies in the elastic deformation stage or initial stable crack growth stage and the incident energy is intermediate. For pulverized specimens, the fracture mechanism is transformed into shear/tensile equivalent from tensile-dominated mixed mode as the pre-stress increases. Specimens with 75 MPa pre-stress release strain energy during failure process, contrary to specimens with lower pre-stresses absorbing energy from outside. The crushing degree of pulverized specimens exhibits a positive correlation with the pre-stress as a consequence of higher damage development in rock.</description><identifier>ISSN: 0723-2632</identifier><identifier>EISSN: 1434-453X</identifier><identifier>DOI: 10.1007/s00603-019-01980-9</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Axial stress ; Civil Engineering ; Compression ; Compressive strength ; Correlation ; Crack propagation ; Defects ; Deformation ; Digital imaging ; Dynamic response ; Earth and Environmental Science ; Earth Sciences ; Elastic deformation ; Energy ; Energy absorption ; Fracture mechanics ; Geophysics/Geodesy ; Growth stage ; High speed cameras ; Impact tests ; Original Paper ; Rockbursts ; Rocks ; Sandstone ; Sedimentary rocks ; Size distribution ; Split Hopkinson pressure bars ; Stone ; Strain ; Strain rate</subject><ispartof>Rock mechanics and rock engineering, 2020-03, Vol.53 (3), p.1305-1331</ispartof><rights>Springer-Verlag GmbH Austria, part of Springer Nature 2019</rights><rights>Rock Mechanics and Rock Engineering is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-be3d33f185b4e33eeda068763461073b7ec2b52226ae5f825324e53484e6d2b73</citedby><cites>FETCH-LOGICAL-a342t-be3d33f185b4e33eeda068763461073b7ec2b52226ae5f825324e53484e6d2b73</cites><orcidid>0000-0002-3905-5514</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00603-019-01980-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00603-019-01980-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Zhou, Zilong</creatorcontrib><creatorcontrib>Cai, Xin</creatorcontrib><creatorcontrib>Li, Xibing</creatorcontrib><creatorcontrib>Cao, Wenzhuo</creatorcontrib><creatorcontrib>Du, Xueming</creatorcontrib><title>Dynamic Response and Energy Evolution of Sandstone Under Coupled Static–Dynamic Compression: Insights from Experimental Study into Deep Rock Engineering Applications</title><title>Rock mechanics and rock engineering</title><addtitle>Rock Mech Rock Eng</addtitle><description>To deeply understand the rock failure characteristics under actual engineering condition, in which static geo-stress and dynamic disturbance usually act simultaneously, impact tests were conducted on sandstone subjected to axial static pre-stresses varying from 0 to 75 MPa by a modified split Hopkinson pressure bar. The fracturing process of specimens was recorded by a high speed camera. Dynamic parameters of sandstone, such as strain rate, dynamic strength and energy partition were acquired. Fracture mechanisms of pulverized specimens were identified by the method combining the displacement trend line and digital image correlation technique. Moreover, fragments of failed specimens were sieved to obtain the fragment size distribution. Test results revealed that, under the same incident energy, the dynamic compressive strength increases first, then decreases slowly and at last drops rapidly with the increase of pre-stress, and reaches the maximum under 24.4% of uniaxial compressive strength due to the closure of initial defects. Four final patterns were observed, namely intact, axial split, rock burst, and pulverization. The rock burst only occurs when the pre-stress lies in the elastic deformation stage or initial stable crack growth stage and the incident energy is intermediate. For pulverized specimens, the fracture mechanism is transformed into shear/tensile equivalent from tensile-dominated mixed mode as the pre-stress increases. Specimens with 75 MPa pre-stress release strain energy during failure process, contrary to specimens with lower pre-stresses absorbing energy from outside. The crushing degree of pulverized specimens exhibits a positive correlation with the pre-stress as a consequence of higher damage development in rock.</description><subject>Axial stress</subject><subject>Civil Engineering</subject><subject>Compression</subject><subject>Compressive strength</subject><subject>Correlation</subject><subject>Crack propagation</subject><subject>Defects</subject><subject>Deformation</subject><subject>Digital imaging</subject><subject>Dynamic response</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Elastic deformation</subject><subject>Energy</subject><subject>Energy absorption</subject><subject>Fracture mechanics</subject><subject>Geophysics/Geodesy</subject><subject>Growth stage</subject><subject>High speed cameras</subject><subject>Impact tests</subject><subject>Original Paper</subject><subject>Rockbursts</subject><subject>Rocks</subject><subject>Sandstone</subject><subject>Sedimentary rocks</subject><subject>Size distribution</subject><subject>Split Hopkinson pressure bars</subject><subject>Stone</subject><subject>Strain</subject><subject>Strain rate</subject><issn>0723-2632</issn><issn>1434-453X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kU1u2zAQhYmgAeImvUBXBLpWQ3Gov-4M200MBAgQ10B3BCWNXLkyyZJUUO9yhxwi98pJQsctsstiMIt535sZPEI-p-xrylhx6RnLGSQsrQ5VsqQ6IZNUgEhEBj8_kAkrOCQ8B35GPnq_ZSwOi3JCnuZ7rXZ9Q-_QW6M9UqVbutDoNnu6uDfDGHqjqenoKg58MBrpWrfo6MyMdsCWroIKffP88PjfaWZ21qH3kftGl9r3m1_B086ZHV38tej6HeqghgiO7Z72Ohg6R7T0zjS_4-ZNrzGK9IZOrR36Rh0O8BfktFODx0__-jlZf1_8mF0nN7dXy9n0JlEgeEhqhBagS8usFgiA2CqWl0UOIk9ZAXWBDa8zznmuMOtKngEXmIEoBeYtrws4J1-OvtaZPyP6ILdmdDqulJxXVc5FmYmo4kdV44z3Djtp41vK7WXK5CEQeQxExjDkayCyihAcIW8P76F7s36HegHaZ5IF</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Zhou, Zilong</creator><creator>Cai, Xin</creator><creator>Li, Xibing</creator><creator>Cao, Wenzhuo</creator><creator>Du, Xueming</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><orcidid>https://orcid.org/0000-0002-3905-5514</orcidid></search><sort><creationdate>20200301</creationdate><title>Dynamic Response and Energy Evolution of Sandstone Under Coupled Static–Dynamic Compression: Insights from Experimental Study into Deep Rock Engineering Applications</title><author>Zhou, Zilong ; Cai, Xin ; Li, Xibing ; Cao, Wenzhuo ; Du, Xueming</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-be3d33f185b4e33eeda068763461073b7ec2b52226ae5f825324e53484e6d2b73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Axial stress</topic><topic>Civil Engineering</topic><topic>Compression</topic><topic>Compressive strength</topic><topic>Correlation</topic><topic>Crack propagation</topic><topic>Defects</topic><topic>Deformation</topic><topic>Digital imaging</topic><topic>Dynamic response</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Elastic deformation</topic><topic>Energy</topic><topic>Energy absorption</topic><topic>Fracture mechanics</topic><topic>Geophysics/Geodesy</topic><topic>Growth stage</topic><topic>High speed cameras</topic><topic>Impact tests</topic><topic>Original Paper</topic><topic>Rockbursts</topic><topic>Rocks</topic><topic>Sandstone</topic><topic>Sedimentary rocks</topic><topic>Size distribution</topic><topic>Split Hopkinson pressure bars</topic><topic>Stone</topic><topic>Strain</topic><topic>Strain rate</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhou, Zilong</creatorcontrib><creatorcontrib>Cai, Xin</creatorcontrib><creatorcontrib>Li, Xibing</creatorcontrib><creatorcontrib>Cao, Wenzhuo</creatorcontrib><creatorcontrib>Du, Xueming</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>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 Korea</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>Science Database</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>Zhou, Zilong</au><au>Cai, Xin</au><au>Li, Xibing</au><au>Cao, Wenzhuo</au><au>Du, Xueming</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dynamic Response and Energy Evolution of Sandstone Under Coupled Static–Dynamic Compression: Insights from Experimental Study into Deep Rock Engineering Applications</atitle><jtitle>Rock mechanics and rock engineering</jtitle><stitle>Rock Mech Rock Eng</stitle><date>2020-03-01</date><risdate>2020</risdate><volume>53</volume><issue>3</issue><spage>1305</spage><epage>1331</epage><pages>1305-1331</pages><issn>0723-2632</issn><eissn>1434-453X</eissn><abstract>To deeply understand the rock failure characteristics under actual engineering condition, in which static geo-stress and dynamic disturbance usually act simultaneously, impact tests were conducted on sandstone subjected to axial static pre-stresses varying from 0 to 75 MPa by a modified split Hopkinson pressure bar. The fracturing process of specimens was recorded by a high speed camera. Dynamic parameters of sandstone, such as strain rate, dynamic strength and energy partition were acquired. Fracture mechanisms of pulverized specimens were identified by the method combining the displacement trend line and digital image correlation technique. Moreover, fragments of failed specimens were sieved to obtain the fragment size distribution. Test results revealed that, under the same incident energy, the dynamic compressive strength increases first, then decreases slowly and at last drops rapidly with the increase of pre-stress, and reaches the maximum under 24.4% of uniaxial compressive strength due to the closure of initial defects. Four final patterns were observed, namely intact, axial split, rock burst, and pulverization. The rock burst only occurs when the pre-stress lies in the elastic deformation stage or initial stable crack growth stage and the incident energy is intermediate. For pulverized specimens, the fracture mechanism is transformed into shear/tensile equivalent from tensile-dominated mixed mode as the pre-stress increases. Specimens with 75 MPa pre-stress release strain energy during failure process, contrary to specimens with lower pre-stresses absorbing energy from outside. The crushing degree of pulverized specimens exhibits a positive correlation with the pre-stress as a consequence of higher damage development in rock.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00603-019-01980-9</doi><tpages>27</tpages><orcidid>https://orcid.org/0000-0002-3905-5514</orcidid></addata></record> |
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subjects | Axial stress Civil Engineering Compression Compressive strength Correlation Crack propagation Defects Deformation Digital imaging Dynamic response Earth and Environmental Science Earth Sciences Elastic deformation Energy Energy absorption Fracture mechanics Geophysics/Geodesy Growth stage High speed cameras Impact tests Original Paper Rockbursts Rocks Sandstone Sedimentary rocks Size distribution Split Hopkinson pressure bars Stone Strain Strain rate |
title | Dynamic Response and Energy Evolution of Sandstone Under Coupled Static–Dynamic Compression: Insights from Experimental Study into Deep Rock Engineering Applications |
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