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Gas-Driven Fracturing of Saturated Granular Media
Physical Review Applied, Volume: 8, Issue: 6
Swansea University Authors: James Campbell, Deren Ozturk, Bjornar Sandnes
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DOI (Published version): 10.1103/physrevapplied.8.064029
Abstract
Multiphase flows in deformable porous materials are important in numerous geological and geotechnical applications, however the complex flow behaviour make subsurface transport processes difficult to control or even characterise. Here we study gas-driven (pneumatic) fracturing of a wet unconsolidate...
Published in: | Physical Review Applied |
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ISSN: | 2331-7019 2331-7019 |
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2017
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2021-01-14T13:01:51.9205222 v2 36781 2017-11-16 Gas-Driven Fracturing of Saturated Granular Media 15b7a72d171aac4c2327a3c7c69dfd92 James Campbell James Campbell true false 14712812fc31e03fc3a3bc9033165beb Deren Ozturk Deren Ozturk true false 61c7c04b5c804d9402caf4881e85234b 0000-0002-4854-5857 Bjornar Sandnes Bjornar Sandnes true false 2017-11-16 EEN Multiphase flows in deformable porous materials are important in numerous geological and geotechnical applications, however the complex flow behaviour make subsurface transport processes difficult to control or even characterise. Here we study gas-driven (pneumatic) fracturing of a wet unconsolidated granular packing confined in a Hele-Shaw cell, and present an in-depth analysis of both pore-scale phenomena and large-scale pattern formation. The process is governed by a complex interplay between pressure, capillary, frictional and viscous forces. At low gas injection rate, fractures grow in a stick-slip fashion and branch out to form a simply connected network. We observe the emergence of a characteristic length-scale -- the separation distance between fracture branches -- creating an apparent uniform spatial fracture density. We conclude that the well defined separation distance is the result of local compaction fronts surrounding fractures, keeping them apart. A scaling argument is presented that predicts fracture density as a function of granular friction, grain size, and capillary interactions. We study the influence of gas injection rate, and find that the system undergoes a fluidisation transition above a critical injection rate, resulting in directional growth of fractures, and a fracture density that increases with increasing rate. A dimensionless Fluidisation number F is defined as the ratio of viscous to frictional forces, and our experiments reveal a frictional regime for F1) characterized by continuous growth in several fracture branches simultaneously. Journal Article Physical Review Applied 8 6 2331-7019 2331-7019 29 12 2017 2017-12-29 10.1103/physrevapplied.8.064029 COLLEGE NANME Engineering COLLEGE CODE EEN Swansea University 2021-01-14T13:01:51.9205222 2017-11-16T09:47:24.1373623 Faculty of Science and Engineering School of Engineering and Applied Sciences - Chemical Engineering James Campbell 1 Deren Ozturk 2 Bjornar Sandnes 0000-0002-4854-5857 3 0036781-16112017095630.pdf Campbell_2017.pdf 2017-11-16T09:56:30.8130000 Output 14215308 application/pdf Accepted Manuscript true 2017-11-16T00:00:00.0000000 true eng |
title |
Gas-Driven Fracturing of Saturated Granular Media |
spellingShingle |
Gas-Driven Fracturing of Saturated Granular Media James Campbell Deren Ozturk Bjornar Sandnes |
title_short |
Gas-Driven Fracturing of Saturated Granular Media |
title_full |
Gas-Driven Fracturing of Saturated Granular Media |
title_fullStr |
Gas-Driven Fracturing of Saturated Granular Media |
title_full_unstemmed |
Gas-Driven Fracturing of Saturated Granular Media |
title_sort |
Gas-Driven Fracturing of Saturated Granular Media |
author_id_str_mv |
15b7a72d171aac4c2327a3c7c69dfd92 14712812fc31e03fc3a3bc9033165beb 61c7c04b5c804d9402caf4881e85234b |
author_id_fullname_str_mv |
15b7a72d171aac4c2327a3c7c69dfd92_***_James Campbell 14712812fc31e03fc3a3bc9033165beb_***_Deren Ozturk 61c7c04b5c804d9402caf4881e85234b_***_Bjornar Sandnes |
author |
James Campbell Deren Ozturk Bjornar Sandnes |
author2 |
James Campbell Deren Ozturk Bjornar Sandnes |
format |
Journal article |
container_title |
Physical Review Applied |
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8 |
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6 |
publishDate |
2017 |
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Swansea University |
issn |
2331-7019 2331-7019 |
doi_str_mv |
10.1103/physrevapplied.8.064029 |
college_str |
Faculty of Science and Engineering |
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facultyofscienceandengineering |
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Faculty of Science and Engineering |
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facultyofscienceandengineering |
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Faculty of Science and Engineering |
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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 |
Multiphase flows in deformable porous materials are important in numerous geological and geotechnical applications, however the complex flow behaviour make subsurface transport processes difficult to control or even characterise. Here we study gas-driven (pneumatic) fracturing of a wet unconsolidated granular packing confined in a Hele-Shaw cell, and present an in-depth analysis of both pore-scale phenomena and large-scale pattern formation. The process is governed by a complex interplay between pressure, capillary, frictional and viscous forces. At low gas injection rate, fractures grow in a stick-slip fashion and branch out to form a simply connected network. We observe the emergence of a characteristic length-scale -- the separation distance between fracture branches -- creating an apparent uniform spatial fracture density. We conclude that the well defined separation distance is the result of local compaction fronts surrounding fractures, keeping them apart. A scaling argument is presented that predicts fracture density as a function of granular friction, grain size, and capillary interactions. We study the influence of gas injection rate, and find that the system undergoes a fluidisation transition above a critical injection rate, resulting in directional growth of fractures, and a fracture density that increases with increasing rate. A dimensionless Fluidisation number F is defined as the ratio of viscous to frictional forces, and our experiments reveal a frictional regime for F1) characterized by continuous growth in several fracture branches simultaneously. |
published_date |
2017-12-29T03:46:07Z |
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1763752194006319104 |
score |
11.035655 |