Conference Paper/Proceeding/Abstract 1238 views
Modelling stick-slip dynamics in frictional fluids
Geophysical Research Abstracts 15, EGU2013-14040, Volume: 15, Issue: 14040
Swansea University Author: Bjornar Sandnes
Abstract
Dissipative interactions between grains often lead to instabilities and pattern formation in flows involving granularmaterials. This is especially so in wet granular flows, where viscous and capillary forces add to the complexdynamics. In a recent study we found an extraordinary diversity in the flo...
Published in: | Geophysical Research Abstracts 15, EGU2013-14040 |
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2013
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URI: | https://cronfa.swan.ac.uk/Record/cronfa21350 |
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<?xml version="1.0"?><rfc1807><datestamp>2016-08-04T14:11:57.8067791</datestamp><bib-version>v2</bib-version><id>21350</id><entry>2015-05-13</entry><title>Modelling stick-slip dynamics in frictional fluids</title><swanseaauthors><author><sid>61c7c04b5c804d9402caf4881e85234b</sid><ORCID>0000-0002-4854-5857</ORCID><firstname>Bjornar</firstname><surname>Sandnes</surname><name>Bjornar Sandnes</name><active>true</active><ethesisStudent>false</ethesisStudent></author></swanseaauthors><date>2015-05-13</date><deptcode>CHEG</deptcode><abstract>Dissipative interactions between grains often lead to instabilities and pattern formation in flows involving granularmaterials. This is especially so in wet granular flows, where viscous and capillary forces add to the complexdynamics. In a recent study we found an extraordinary diversity in the flow behaviour of wet granular materialdisplaced by air in a Hele-Shaw cell [1]. By varying the air injection rate, system compressibility, and granularmaterial filling fraction, several distinct flow morphologies were observed. The study maps these out in phasediagrams.Here we present a numerical model that focuses on one of the observed pattern transitions; from frictionalfingering to stick-slip bubbles. By incorporating surface tension, pressure and frictional forces, we trace thedisplacement of the interface using a dynamical version of a quasi-static algorithm developed previously [2]. Themodel reproduces the growth and evolution of the flow dynamics, resulting in patterns that closely resemble thoseobserved in the experiments. The numerical scheme offers a method to study the transition between the patternformation modes in detail, complementary to the experimental results.</abstract><type>Conference Paper/Proceeding/Abstract</type><journal>Geophysical Research Abstracts 15, EGU2013-14040</journal><volume>15</volume><journalNumber>14040</journalNumber><publisher/><keywords/><publishedDay>31</publishedDay><publishedMonth>12</publishedMonth><publishedYear>2013</publishedYear><publishedDate>2013-12-31</publishedDate><doi/><url/><notes></notes><college>COLLEGE NANME</college><department>Chemical Engineering</department><CollegeCode>COLLEGE CODE</CollegeCode><DepartmentCode>CHEG</DepartmentCode><institution>Swansea University</institution><apcterm/><lastEdited>2016-08-04T14:11:57.8067791</lastEdited><Created>2015-05-13T10:56:17.5564543</Created><path><level id="1">Faculty of Science and Engineering</level><level id="2">School of Engineering and Applied Sciences - Chemical Engineering</level></path><authors><author><firstname>Jon Alm</firstname><surname>Eriksen</surname><order>1</order></author><author><firstname>Bjornar</firstname><surname>Sandnes</surname><orcid>0000-0002-4854-5857</orcid><order>2</order></author><author><firstname>Knut Jorgen</firstname><surname>Maloy</surname><order>3</order></author><author><firstname>Eirik Grude</firstname><surname>Flekkoy</surname><order>4</order></author></authors><documents/><OutputDurs/></rfc1807> |
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2016-08-04T14:11:57.8067791 v2 21350 2015-05-13 Modelling stick-slip dynamics in frictional fluids 61c7c04b5c804d9402caf4881e85234b 0000-0002-4854-5857 Bjornar Sandnes Bjornar Sandnes true false 2015-05-13 CHEG Dissipative interactions between grains often lead to instabilities and pattern formation in flows involving granularmaterials. This is especially so in wet granular flows, where viscous and capillary forces add to the complexdynamics. In a recent study we found an extraordinary diversity in the flow behaviour of wet granular materialdisplaced by air in a Hele-Shaw cell [1]. By varying the air injection rate, system compressibility, and granularmaterial filling fraction, several distinct flow morphologies were observed. The study maps these out in phasediagrams.Here we present a numerical model that focuses on one of the observed pattern transitions; from frictionalfingering to stick-slip bubbles. By incorporating surface tension, pressure and frictional forces, we trace thedisplacement of the interface using a dynamical version of a quasi-static algorithm developed previously [2]. Themodel reproduces the growth and evolution of the flow dynamics, resulting in patterns that closely resemble thoseobserved in the experiments. The numerical scheme offers a method to study the transition between the patternformation modes in detail, complementary to the experimental results. Conference Paper/Proceeding/Abstract Geophysical Research Abstracts 15, EGU2013-14040 15 14040 31 12 2013 2013-12-31 COLLEGE NANME Chemical Engineering COLLEGE CODE CHEG Swansea University 2016-08-04T14:11:57.8067791 2015-05-13T10:56:17.5564543 Faculty of Science and Engineering School of Engineering and Applied Sciences - Chemical Engineering Jon Alm Eriksen 1 Bjornar Sandnes 0000-0002-4854-5857 2 Knut Jorgen Maloy 3 Eirik Grude Flekkoy 4 |
title |
Modelling stick-slip dynamics in frictional fluids |
spellingShingle |
Modelling stick-slip dynamics in frictional fluids Bjornar Sandnes |
title_short |
Modelling stick-slip dynamics in frictional fluids |
title_full |
Modelling stick-slip dynamics in frictional fluids |
title_fullStr |
Modelling stick-slip dynamics in frictional fluids |
title_full_unstemmed |
Modelling stick-slip dynamics in frictional fluids |
title_sort |
Modelling stick-slip dynamics in frictional fluids |
author_id_str_mv |
61c7c04b5c804d9402caf4881e85234b |
author_id_fullname_str_mv |
61c7c04b5c804d9402caf4881e85234b_***_Bjornar Sandnes |
author |
Bjornar Sandnes |
author2 |
Jon Alm Eriksen Bjornar Sandnes Knut Jorgen Maloy Eirik Grude Flekkoy |
format |
Conference Paper/Proceeding/Abstract |
container_title |
Geophysical Research Abstracts 15, EGU2013-14040 |
container_volume |
15 |
container_issue |
14040 |
publishDate |
2013 |
institution |
Swansea University |
college_str |
Faculty of Science and Engineering |
hierarchytype |
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facultyofscienceandengineering |
hierarchy_top_title |
Faculty of Science and Engineering |
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facultyofscienceandengineering |
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Faculty of Science and Engineering |
department_str |
School of Engineering and Applied Sciences - Chemical Engineering{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Engineering and Applied Sciences - Chemical Engineering |
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description |
Dissipative interactions between grains often lead to instabilities and pattern formation in flows involving granularmaterials. This is especially so in wet granular flows, where viscous and capillary forces add to the complexdynamics. In a recent study we found an extraordinary diversity in the flow behaviour of wet granular materialdisplaced by air in a Hele-Shaw cell [1]. By varying the air injection rate, system compressibility, and granularmaterial filling fraction, several distinct flow morphologies were observed. The study maps these out in phasediagrams.Here we present a numerical model that focuses on one of the observed pattern transitions; from frictionalfingering to stick-slip bubbles. By incorporating surface tension, pressure and frictional forces, we trace thedisplacement of the interface using a dynamical version of a quasi-static algorithm developed previously [2]. Themodel reproduces the growth and evolution of the flow dynamics, resulting in patterns that closely resemble thoseobserved in the experiments. The numerical scheme offers a method to study the transition between the patternformation modes in detail, complementary to the experimental results. |
published_date |
2013-12-31T03:25:18Z |
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1763750883854647296 |
score |
11.036815 |