Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method
The dynamic behavior of filled joints is mostly controlled by the filled medium. In addition to nonlinear elastic behavior, viscoelastic behavior of filled joints is also of great significance. Here, a theoretical study of stress wave propagation through a filled rock joint with linear viscoelastic...
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Veröffentlicht in: | Rock mechanics and rock engineering 2017-12, Vol.50 (12), p.3197-3207 |
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description | The dynamic behavior of filled joints is mostly controlled by the filled medium. In addition to nonlinear elastic behavior, viscoelastic behavior of filled joints is also of great significance. Here, a theoretical study of stress wave propagation through a filled rock joint with linear viscoelastic deformation behavior has been carried out using a modified time-domain recursive method (TDRM). A displacement discontinuity model was extended to form a displacement and stress discontinuity model, and the differential constitutive relationship of viscoelastic model was adopted to introduce the mass and viscoelastic behavior of filled medium. A standard linear solid model, which can be degenerated into the Kelvin and Maxwell models, was adopted in deriving this method. Transmission and reflection coefficients were adopted to verify this method. Besides, the effects of some parameters on wave propagation across a filled rock joint with linear viscoelastic deformation behavior were discussed. Then, a comparison of the time-history curves calculated by the present method with those by frequency-domain method (FDM) was performed. The results indicated that change tendencies of the transmission and reflection coefficients for these viscoelastic models versus incident angle were the same as each other but not frequency. The mass and viscosity coupling of filled medium did not fundamentally change wave propagation. The modified TDRM was found to be more efficient than the FDM. |
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In addition to nonlinear elastic behavior, viscoelastic behavior of filled joints is also of great significance. Here, a theoretical study of stress wave propagation through a filled rock joint with linear viscoelastic deformation behavior has been carried out using a modified time-domain recursive method (TDRM). A displacement discontinuity model was extended to form a displacement and stress discontinuity model, and the differential constitutive relationship of viscoelastic model was adopted to introduce the mass and viscoelastic behavior of filled medium. A standard linear solid model, which can be degenerated into the Kelvin and Maxwell models, was adopted in deriving this method. Transmission and reflection coefficients were adopted to verify this method. Besides, the effects of some parameters on wave propagation across a filled rock joint with linear viscoelastic deformation behavior were discussed. Then, a comparison of the time-history curves calculated by the present method with those by frequency-domain method (FDM) was performed. The results indicated that change tendencies of the transmission and reflection coefficients for these viscoelastic models versus incident angle were the same as each other but not frequency. The mass and viscosity coupling of filled medium did not fundamentally change wave propagation. The modified TDRM was found to be more efficient than the FDM.</description><identifier>ISSN: 0723-2632</identifier><identifier>EISSN: 1434-453X</identifier><identifier>DOI: 10.1007/s00603-017-1301-4</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Civil Engineering ; Coefficients ; Constitutive relationships ; Deformation ; Discontinuity ; Displacement ; Earth and Environmental Science ; Earth Sciences ; Elasticity ; Geophysics/Geodesy ; History ; Joints ; Joints (timber) ; Mathematical models ; Original Paper ; Propagation ; Recursive methods ; Reflection ; Rocks ; Stress analysis ; Stress propagation ; Time ; Time domain analysis ; Viscoelasticity ; Viscosity ; Wave propagation</subject><ispartof>Rock mechanics and rock engineering, 2017-12, Vol.50 (12), p.3197-3207</ispartof><rights>Springer-Verlag GmbH Austria 2017</rights><rights>Rock Mechanics and Rock Engineering is a copyright of Springer, (2017). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-8d043ab317bae9973f6cca8131e807d97f2054ee3e459775c6af35b6cdf6ac173</citedby><cites>FETCH-LOGICAL-a339t-8d043ab317bae9973f6cca8131e807d97f2054ee3e459775c6af35b6cdf6ac173</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/s00603-017-1301-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00603-017-1301-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Wang, Rui</creatorcontrib><creatorcontrib>Hu, Zhiping</creatorcontrib><creatorcontrib>Zhang, Dan</creatorcontrib><creatorcontrib>Wang, Qiyao</creatorcontrib><title>Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method</title><title>Rock mechanics and rock engineering</title><addtitle>Rock Mech Rock Eng</addtitle><description>The dynamic behavior of filled joints is mostly controlled by the filled medium. In addition to nonlinear elastic behavior, viscoelastic behavior of filled joints is also of great significance. Here, a theoretical study of stress wave propagation through a filled rock joint with linear viscoelastic deformation behavior has been carried out using a modified time-domain recursive method (TDRM). A displacement discontinuity model was extended to form a displacement and stress discontinuity model, and the differential constitutive relationship of viscoelastic model was adopted to introduce the mass and viscoelastic behavior of filled medium. A standard linear solid model, which can be degenerated into the Kelvin and Maxwell models, was adopted in deriving this method. Transmission and reflection coefficients were adopted to verify this method. Besides, the effects of some parameters on wave propagation across a filled rock joint with linear viscoelastic deformation behavior were discussed. Then, a comparison of the time-history curves calculated by the present method with those by frequency-domain method (FDM) was performed. The results indicated that change tendencies of the transmission and reflection coefficients for these viscoelastic models versus incident angle were the same as each other but not frequency. The mass and viscosity coupling of filled medium did not fundamentally change wave propagation. The modified TDRM was found to be more efficient than the FDM.</description><subject>Civil Engineering</subject><subject>Coefficients</subject><subject>Constitutive relationships</subject><subject>Deformation</subject><subject>Discontinuity</subject><subject>Displacement</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Elasticity</subject><subject>Geophysics/Geodesy</subject><subject>History</subject><subject>Joints</subject><subject>Joints (timber)</subject><subject>Mathematical models</subject><subject>Original Paper</subject><subject>Propagation</subject><subject>Recursive methods</subject><subject>Reflection</subject><subject>Rocks</subject><subject>Stress analysis</subject><subject>Stress propagation</subject><subject>Time</subject><subject>Time domain analysis</subject><subject>Viscoelasticity</subject><subject>Viscosity</subject><subject>Wave propagation</subject><issn>0723-2632</issn><issn>1434-453X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kLtOwzAUhi0EEqXwAGyWmA12nMTJCIVyUREIWmCzXOekcdXExXaKeAMem5QwsDAd6T__RfoQOmb0lFEqzjylKeWEMkEYp4zEO2jAYh6TOOFvu2hARcRJlPJoHx14v6S0e4psgL4enV2rhQrGNtiWOFSAn4MD7_Gr2gCeVs62i-pHH5vVCgp8Z00T8IcJFZ6YBpTDL8ZrCyvlg9H4Ekrr6r7wAiq1MdbhmTfNAk9NDeTS1so0-Al067zpJu4hVLY4RHulWnk4-r1DNBtfTUc3ZPJwfTs6nxDFeR5IVtCYqzlnYq4gzwUvU61VxjiDjIoiF2VEkxiAQ5zkQiQ6VSVP5qkuylRpJvgQnfS9a2ffW_BBLm3rmm5SsjzNWMKiNO9crHdpZ713UMq1M7Vyn5JRuQUue-CyAy63wGXcZaI-4ztvswD3p_nf0DckdITg</recordid><startdate>20171201</startdate><enddate>20171201</enddate><creator>Wang, Rui</creator><creator>Hu, Zhiping</creator><creator>Zhang, Dan</creator><creator>Wang, Qiyao</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>20171201</creationdate><title>Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method</title><author>Wang, Rui ; Hu, Zhiping ; Zhang, Dan ; Wang, Qiyao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-8d043ab317bae9973f6cca8131e807d97f2054ee3e459775c6af35b6cdf6ac173</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Civil Engineering</topic><topic>Coefficients</topic><topic>Constitutive relationships</topic><topic>Deformation</topic><topic>Discontinuity</topic><topic>Displacement</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Elasticity</topic><topic>Geophysics/Geodesy</topic><topic>History</topic><topic>Joints</topic><topic>Joints (timber)</topic><topic>Mathematical models</topic><topic>Original Paper</topic><topic>Propagation</topic><topic>Recursive methods</topic><topic>Reflection</topic><topic>Rocks</topic><topic>Stress analysis</topic><topic>Stress propagation</topic><topic>Time</topic><topic>Time domain analysis</topic><topic>Viscoelasticity</topic><topic>Viscosity</topic><topic>Wave propagation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Rui</creatorcontrib><creatorcontrib>Hu, Zhiping</creatorcontrib><creatorcontrib>Zhang, Dan</creatorcontrib><creatorcontrib>Wang, Qiyao</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 (ProQuest)</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>Wang, Rui</au><au>Hu, Zhiping</au><au>Zhang, Dan</au><au>Wang, Qiyao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method</atitle><jtitle>Rock mechanics and rock engineering</jtitle><stitle>Rock Mech Rock Eng</stitle><date>2017-12-01</date><risdate>2017</risdate><volume>50</volume><issue>12</issue><spage>3197</spage><epage>3207</epage><pages>3197-3207</pages><issn>0723-2632</issn><eissn>1434-453X</eissn><abstract>The dynamic behavior of filled joints is mostly controlled by the filled medium. In addition to nonlinear elastic behavior, viscoelastic behavior of filled joints is also of great significance. Here, a theoretical study of stress wave propagation through a filled rock joint with linear viscoelastic deformation behavior has been carried out using a modified time-domain recursive method (TDRM). A displacement discontinuity model was extended to form a displacement and stress discontinuity model, and the differential constitutive relationship of viscoelastic model was adopted to introduce the mass and viscoelastic behavior of filled medium. A standard linear solid model, which can be degenerated into the Kelvin and Maxwell models, was adopted in deriving this method. Transmission and reflection coefficients were adopted to verify this method. Besides, the effects of some parameters on wave propagation across a filled rock joint with linear viscoelastic deformation behavior were discussed. Then, a comparison of the time-history curves calculated by the present method with those by frequency-domain method (FDM) was performed. The results indicated that change tendencies of the transmission and reflection coefficients for these viscoelastic models versus incident angle were the same as each other but not frequency. The mass and viscosity coupling of filled medium did not fundamentally change wave propagation. The modified TDRM was found to be more efficient than the FDM.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00603-017-1301-4</doi><tpages>11</tpages></addata></record> |
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subjects | Civil Engineering Coefficients Constitutive relationships Deformation Discontinuity Displacement Earth and Environmental Science Earth Sciences Elasticity Geophysics/Geodesy History Joints Joints (timber) Mathematical models Original Paper Propagation Recursive methods Reflection Rocks Stress analysis Stress propagation Time Time domain analysis Viscoelasticity Viscosity Wave propagation |
title | Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method |
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