Simplest deformation models of a fluid-saturated poroelastic medium

Under analysis is the model of two-phase flow in porous medium and deformation of the pore space. The model includes the equations of fluid transfer and porous matrix deformation, derived from the conservation laws. It is shown that the system of the constitutive equations contains a few small param...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of mining science 2014-03, Vol.50 (2), p.235-248
Hauptverfasser: Bocharov, O. B., Rudyak, V. Ya, Seryakov, A. V.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 248
container_issue 2
container_start_page 235
container_title Journal of mining science
container_volume 50
creator Bocharov, O. B.
Rudyak, V. Ya
Seryakov, A. V.
description Under analysis is the model of two-phase flow in porous medium and deformation of the pore space. The model includes the equations of fluid transfer and porous matrix deformation, derived from the conservation laws. It is shown that the system of the constitutive equations contains a few small parameters, and the corresponding expansion allows obtaining a hierarchical sequence of models of certain deformation conditions. The zero approximation and first approximation models are written in explicit form. It is found that if fluids are incompressible, the first approximation equations go to the Buckley-Leverett model-like system with account for the change of the porous space. The zero approximation equations describe the porous medium behavior under condition of the unchanged volume. In this case, the equation of the pore pressure is separated from the equation of the elastic matrix. The analytical solutions obtained for the zero approximation model in cylindrical coordinates feature shear stresses capable to cause failure.
doi_str_mv 10.1134/S1062739114020057
format Article
fullrecord <record><control><sourceid>gale_cross</sourceid><recordid>TN_cdi_gale_infotracacademiconefile_A384543626</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A384543626</galeid><sourcerecordid>A384543626</sourcerecordid><originalsourceid>FETCH-LOGICAL-c361t-36b4a67d0680de8304d5ca5620dc53eb0ffca89f25221b42ed2433232e7b63d93</originalsourceid><addsrcrecordid>eNp9kE1LAzEQhoMoWKs_wFuuHrbma7O7x1L8KBQEq-clm0xKyu6mJFnQf29KvRRB5jDDzPPM4UXonpIFpVw8bimRrOINpYIwQsrqAs1oWfGirri8zHM-F8f7NbqJcU8IaWrZzNBq64ZDDzFhA9aHQSXnRzx4A33E3mKFbT85U0SVpqASGHzwwUOvYnIaD2DcNNyiK6v6CHe_fY4-n58-Vq_F5u1lvVpuCs0lTQWXnVCyMkTWxEDNiTClVqVkxOiSQ0es1apuLCsZo51gYJjgnHEGVSe5afgcLU5_d6qH1o3Wp6B0LgOD034E6_J-yWtRCi6ZzMLDmZCZBF9pp6YY2_X2_ZylJ1YHH2MA2x6CG1T4bilpjxG3fyLODjs5MbPjDkK791MYcwb_SD9R13xL</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Simplest deformation models of a fluid-saturated poroelastic medium</title><source>Springer Nature - Complete Springer Journals</source><creator>Bocharov, O. B. ; Rudyak, V. Ya ; Seryakov, A. V.</creator><creatorcontrib>Bocharov, O. B. ; Rudyak, V. Ya ; Seryakov, A. V.</creatorcontrib><description>Under analysis is the model of two-phase flow in porous medium and deformation of the pore space. The model includes the equations of fluid transfer and porous matrix deformation, derived from the conservation laws. It is shown that the system of the constitutive equations contains a few small parameters, and the corresponding expansion allows obtaining a hierarchical sequence of models of certain deformation conditions. The zero approximation and first approximation models are written in explicit form. It is found that if fluids are incompressible, the first approximation equations go to the Buckley-Leverett model-like system with account for the change of the porous space. The zero approximation equations describe the porous medium behavior under condition of the unchanged volume. In this case, the equation of the pore pressure is separated from the equation of the elastic matrix. The analytical solutions obtained for the zero approximation model in cylindrical coordinates feature shear stresses capable to cause failure.</description><identifier>ISSN: 1062-7391</identifier><identifier>EISSN: 1573-8736</identifier><identifier>DOI: 10.1134/S1062739114020057</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Analysis ; Earth and Environmental Science ; Earth Sciences ; Environmental law ; Geomechanics ; Geophysics/Geodesy ; Geotechnical Engineering &amp; Applied Earth Sciences ; Mineral Resources</subject><ispartof>Journal of mining science, 2014-03, Vol.50 (2), p.235-248</ispartof><rights>Pleiades Publishing, Ltd. 2014</rights><rights>COPYRIGHT 2014 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c361t-36b4a67d0680de8304d5ca5620dc53eb0ffca89f25221b42ed2433232e7b63d93</citedby><cites>FETCH-LOGICAL-c361t-36b4a67d0680de8304d5ca5620dc53eb0ffca89f25221b42ed2433232e7b63d93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1062739114020057$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1062739114020057$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Bocharov, O. B.</creatorcontrib><creatorcontrib>Rudyak, V. Ya</creatorcontrib><creatorcontrib>Seryakov, A. V.</creatorcontrib><title>Simplest deformation models of a fluid-saturated poroelastic medium</title><title>Journal of mining science</title><addtitle>J Min Sci</addtitle><description>Under analysis is the model of two-phase flow in porous medium and deformation of the pore space. The model includes the equations of fluid transfer and porous matrix deformation, derived from the conservation laws. It is shown that the system of the constitutive equations contains a few small parameters, and the corresponding expansion allows obtaining a hierarchical sequence of models of certain deformation conditions. The zero approximation and first approximation models are written in explicit form. It is found that if fluids are incompressible, the first approximation equations go to the Buckley-Leverett model-like system with account for the change of the porous space. The zero approximation equations describe the porous medium behavior under condition of the unchanged volume. In this case, the equation of the pore pressure is separated from the equation of the elastic matrix. The analytical solutions obtained for the zero approximation model in cylindrical coordinates feature shear stresses capable to cause failure.</description><subject>Analysis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental law</subject><subject>Geomechanics</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering &amp; Applied Earth Sciences</subject><subject>Mineral Resources</subject><issn>1062-7391</issn><issn>1573-8736</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWKs_wFuuHrbma7O7x1L8KBQEq-clm0xKyu6mJFnQf29KvRRB5jDDzPPM4UXonpIFpVw8bimRrOINpYIwQsrqAs1oWfGirri8zHM-F8f7NbqJcU8IaWrZzNBq64ZDDzFhA9aHQSXnRzx4A33E3mKFbT85U0SVpqASGHzwwUOvYnIaD2DcNNyiK6v6CHe_fY4-n58-Vq_F5u1lvVpuCs0lTQWXnVCyMkTWxEDNiTClVqVkxOiSQ0es1apuLCsZo51gYJjgnHEGVSe5afgcLU5_d6qH1o3Wp6B0LgOD034E6_J-yWtRCi6ZzMLDmZCZBF9pp6YY2_X2_ZylJ1YHH2MA2x6CG1T4bilpjxG3fyLODjs5MbPjDkK791MYcwb_SD9R13xL</recordid><startdate>20140301</startdate><enddate>20140301</enddate><creator>Bocharov, O. B.</creator><creator>Rudyak, V. Ya</creator><creator>Seryakov, A. V.</creator><general>Pleiades Publishing</general><general>Springer</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope></search><sort><creationdate>20140301</creationdate><title>Simplest deformation models of a fluid-saturated poroelastic medium</title><author>Bocharov, O. B. ; Rudyak, V. Ya ; Seryakov, A. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c361t-36b4a67d0680de8304d5ca5620dc53eb0ffca89f25221b42ed2433232e7b63d93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Analysis</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental law</topic><topic>Geomechanics</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering &amp; Applied Earth Sciences</topic><topic>Mineral Resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bocharov, O. B.</creatorcontrib><creatorcontrib>Rudyak, V. Ya</creatorcontrib><creatorcontrib>Seryakov, A. V.</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Science</collection><jtitle>Journal of mining science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bocharov, O. B.</au><au>Rudyak, V. Ya</au><au>Seryakov, A. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Simplest deformation models of a fluid-saturated poroelastic medium</atitle><jtitle>Journal of mining science</jtitle><stitle>J Min Sci</stitle><date>2014-03-01</date><risdate>2014</risdate><volume>50</volume><issue>2</issue><spage>235</spage><epage>248</epage><pages>235-248</pages><issn>1062-7391</issn><eissn>1573-8736</eissn><abstract>Under analysis is the model of two-phase flow in porous medium and deformation of the pore space. The model includes the equations of fluid transfer and porous matrix deformation, derived from the conservation laws. It is shown that the system of the constitutive equations contains a few small parameters, and the corresponding expansion allows obtaining a hierarchical sequence of models of certain deformation conditions. The zero approximation and first approximation models are written in explicit form. It is found that if fluids are incompressible, the first approximation equations go to the Buckley-Leverett model-like system with account for the change of the porous space. The zero approximation equations describe the porous medium behavior under condition of the unchanged volume. In this case, the equation of the pore pressure is separated from the equation of the elastic matrix. The analytical solutions obtained for the zero approximation model in cylindrical coordinates feature shear stresses capable to cause failure.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1062739114020057</doi><tpages>14</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1062-7391
ispartof Journal of mining science, 2014-03, Vol.50 (2), p.235-248
issn 1062-7391
1573-8736
language eng
recordid cdi_gale_infotracacademiconefile_A384543626
source Springer Nature - Complete Springer Journals
subjects Analysis
Earth and Environmental Science
Earth Sciences
Environmental law
Geomechanics
Geophysics/Geodesy
Geotechnical Engineering & Applied Earth Sciences
Mineral Resources
title Simplest deformation models of a fluid-saturated poroelastic medium
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T08%3A40%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Simplest%20deformation%20models%20of%20a%20fluid-saturated%20poroelastic%20medium&rft.jtitle=Journal%20of%20mining%20science&rft.au=Bocharov,%20O.%20B.&rft.date=2014-03-01&rft.volume=50&rft.issue=2&rft.spage=235&rft.epage=248&rft.pages=235-248&rft.issn=1062-7391&rft.eissn=1573-8736&rft_id=info:doi/10.1134/S1062739114020057&rft_dat=%3Cgale_cross%3EA384543626%3C/gale_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_galeid=A384543626&rfr_iscdi=true