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Roughness Control on Multiphase Flow in Rock Fractures
The roughness of rock fractures induces irregular flow passages and significantly affects the displacement front. Previous studies focus on displacement instabilities in porous media, but how roughness controls displacement patterns in rock fractures remains unclear. Here, we derive a theoretical mo...
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Published in: | Geophysical research letters 2019-11, Vol.46 (21), p.12002-12011 |
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description | The roughness of rock fractures induces irregular flow passages and significantly affects the displacement front. Previous studies focus on displacement instabilities in porous media, but how roughness controls displacement patterns in rock fractures remains unclear. Here, we derive a theoretical model that describes the two transitions of drainage displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by this model exhibits excellent agreement with our experimental results, showing that increasing roughness index λb destabilizes displacement fronts. We further find that in capillary fingering regime the percentage of dissipated energy to the total external work increases from 39% to 61% as λb increases from 0.082 to 0.245. Our work elucidates the mechanism of roughness control on multiphase flow in fractures and provides a basis for developing a rigorous upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Plain Language Summary
Multiphase flow in fractured media is an important process involved in many natural processes and subsurface engineering applications. Geological fractures are inherently rough to various degrees. The roughness of rock fracture, inducing irregular flow passages, plays a fundamental role in the displacement of one fluid by another immiscible one. Despite its importance, how the roughness controls the displacement patterns remains poorly understood. Here, we propose a theoretical model to quantify the impact of displacement patterns, which describes the two transitions of displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by the theoretical model is in excellent agreement with our experimental results. We also find that higher roughness index λb causes more dissipated energy. The dissipation ratio, representing the percentage of dissipated energy to the external work, increases from 39% to 61% as λb increases from 0.082 to 0.245 in the capillary fingering regime. Our work proposes a phase diagram to elucidate the impact of roughness on multiphase flow that is previously not reported; it also provides a basis for an upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Key Points
A theoretical model is proposed to describe the two trans |
doi_str_mv | 10.1029/2019GL084762 |
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Plain Language Summary
Multiphase flow in fractured media is an important process involved in many natural processes and subsurface engineering applications. Geological fractures are inherently rough to various degrees. The roughness of rock fracture, inducing irregular flow passages, plays a fundamental role in the displacement of one fluid by another immiscible one. Despite its importance, how the roughness controls the displacement patterns remains poorly understood. Here, we propose a theoretical model to quantify the impact of displacement patterns, which describes the two transitions of displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by the theoretical model is in excellent agreement with our experimental results. We also find that higher roughness index λb causes more dissipated energy. The dissipation ratio, representing the percentage of dissipated energy to the external work, increases from 39% to 61% as λb increases from 0.082 to 0.245 in the capillary fingering regime. Our work proposes a phase diagram to elucidate the impact of roughness on multiphase flow that is previously not reported; it also provides a basis for an upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Key Points
A theoretical model is proposed to describe the two transitions of displacement patterns in rock fractures as functions of roughness
The phase diagram predicted by the model agrees very well with experiments, showing a destabilizing effect of roughness on fronts
As roughness index increases, the ratio of dissipated energy to external work increases from 39% to 61% in the capillary fingering regime</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2019GL084762</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Displacement ; displacement pattern ; Energy dissipation ; Energy exchange ; Fractures ; Fronts ; Methods ; Multiphase flow ; phase diagram ; Phase diagrams ; Porous media ; rock fractures ; Rocks ; Roughness</subject><ispartof>Geophysical research letters, 2019-11, Vol.46 (21), p.12002-12011</ispartof><rights>2019. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3293-89e192647337de4e2a700668d9c503b6ff580b7133f29ec5dff17209d6c4c2c93</citedby><cites>FETCH-LOGICAL-a3293-89e192647337de4e2a700668d9c503b6ff580b7133f29ec5dff17209d6c4c2c93</cites><orcidid>0000-0002-2296-050X ; 0000-0001-9104-4401 ; 0000-0002-5685-0819 ; 0000-0003-2328-7035</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2019GL084762$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2019GL084762$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,777,781,11495,27905,27906,46449,46873</link.rule.ids></links><search><creatorcontrib>Hu, Ran</creatorcontrib><creatorcontrib>Zhou, Chen‐Xing</creatorcontrib><creatorcontrib>Wu, Dong‐Sheng</creatorcontrib><creatorcontrib>Yang, Zhibing</creatorcontrib><creatorcontrib>Chen, Yi‐Feng</creatorcontrib><title>Roughness Control on Multiphase Flow in Rock Fractures</title><title>Geophysical research letters</title><description>The roughness of rock fractures induces irregular flow passages and significantly affects the displacement front. Previous studies focus on displacement instabilities in porous media, but how roughness controls displacement patterns in rock fractures remains unclear. Here, we derive a theoretical model that describes the two transitions of drainage displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by this model exhibits excellent agreement with our experimental results, showing that increasing roughness index λb destabilizes displacement fronts. We further find that in capillary fingering regime the percentage of dissipated energy to the total external work increases from 39% to 61% as λb increases from 0.082 to 0.245. Our work elucidates the mechanism of roughness control on multiphase flow in fractures and provides a basis for developing a rigorous upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Plain Language Summary
Multiphase flow in fractured media is an important process involved in many natural processes and subsurface engineering applications. Geological fractures are inherently rough to various degrees. The roughness of rock fracture, inducing irregular flow passages, plays a fundamental role in the displacement of one fluid by another immiscible one. Despite its importance, how the roughness controls the displacement patterns remains poorly understood. Here, we propose a theoretical model to quantify the impact of displacement patterns, which describes the two transitions of displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by the theoretical model is in excellent agreement with our experimental results. We also find that higher roughness index λb causes more dissipated energy. The dissipation ratio, representing the percentage of dissipated energy to the external work, increases from 39% to 61% as λb increases from 0.082 to 0.245 in the capillary fingering regime. Our work proposes a phase diagram to elucidate the impact of roughness on multiphase flow that is previously not reported; it also provides a basis for an upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Key Points
A theoretical model is proposed to describe the two transitions of displacement patterns in rock fractures as functions of roughness
The phase diagram predicted by the model agrees very well with experiments, showing a destabilizing effect of roughness on fronts
As roughness index increases, the ratio of dissipated energy to external work increases from 39% to 61% in the capillary fingering regime</description><subject>Displacement</subject><subject>displacement pattern</subject><subject>Energy dissipation</subject><subject>Energy exchange</subject><subject>Fractures</subject><subject>Fronts</subject><subject>Methods</subject><subject>Multiphase flow</subject><subject>phase diagram</subject><subject>Phase diagrams</subject><subject>Porous media</subject><subject>rock fractures</subject><subject>Rocks</subject><subject>Roughness</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kMFLwzAYxYMoOKc3_4CAV6tfkjbpd5ThplARhp5DlyauszY1aRn771epB0-e3jv83nvwCLlmcMeA4z0HhqsC8lRJfkJmDNM0yQHUKZkB4Oi5kufkIsYdAAgQbEbk2g8f29bGSBe-7YNvqG_py9D0dbcto6XLxu9p3dK1N590GUrTD8HGS3Lmyibaq1-dk_fl49viKSleV8-LhyIpBUeR5GgZcpkqIVRlU8tLBSBlXqHJQGykc1kOG8WEcBytySrnmOKAlTSp4QbFnNxMvV3w34ONvd75IbTjpOaCoQKVj-E5uZ0oE3yMwTrdhfqrDAfNQP88o_8-M-J8wvd1Yw__snq1LjJUUogjXftiLA</recordid><startdate>20191116</startdate><enddate>20191116</enddate><creator>Hu, Ran</creator><creator>Zhou, Chen‐Xing</creator><creator>Wu, Dong‐Sheng</creator><creator>Yang, Zhibing</creator><creator>Chen, Yi‐Feng</creator><general>John Wiley & Sons, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-2296-050X</orcidid><orcidid>https://orcid.org/0000-0001-9104-4401</orcidid><orcidid>https://orcid.org/0000-0002-5685-0819</orcidid><orcidid>https://orcid.org/0000-0003-2328-7035</orcidid></search><sort><creationdate>20191116</creationdate><title>Roughness Control on Multiphase Flow in Rock Fractures</title><author>Hu, Ran ; Zhou, Chen‐Xing ; Wu, Dong‐Sheng ; Yang, Zhibing ; Chen, Yi‐Feng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3293-89e192647337de4e2a700668d9c503b6ff580b7133f29ec5dff17209d6c4c2c93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Displacement</topic><topic>displacement pattern</topic><topic>Energy dissipation</topic><topic>Energy exchange</topic><topic>Fractures</topic><topic>Fronts</topic><topic>Methods</topic><topic>Multiphase flow</topic><topic>phase diagram</topic><topic>Phase diagrams</topic><topic>Porous media</topic><topic>rock fractures</topic><topic>Rocks</topic><topic>Roughness</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hu, Ran</creatorcontrib><creatorcontrib>Zhou, Chen‐Xing</creatorcontrib><creatorcontrib>Wu, Dong‐Sheng</creatorcontrib><creatorcontrib>Yang, Zhibing</creatorcontrib><creatorcontrib>Chen, Yi‐Feng</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hu, Ran</au><au>Zhou, Chen‐Xing</au><au>Wu, Dong‐Sheng</au><au>Yang, Zhibing</au><au>Chen, Yi‐Feng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Roughness Control on Multiphase Flow in Rock Fractures</atitle><jtitle>Geophysical research letters</jtitle><date>2019-11-16</date><risdate>2019</risdate><volume>46</volume><issue>21</issue><spage>12002</spage><epage>12011</epage><pages>12002-12011</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The roughness of rock fractures induces irregular flow passages and significantly affects the displacement front. Previous studies focus on displacement instabilities in porous media, but how roughness controls displacement patterns in rock fractures remains unclear. Here, we derive a theoretical model that describes the two transitions of drainage displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by this model exhibits excellent agreement with our experimental results, showing that increasing roughness index λb destabilizes displacement fronts. We further find that in capillary fingering regime the percentage of dissipated energy to the total external work increases from 39% to 61% as λb increases from 0.082 to 0.245. Our work elucidates the mechanism of roughness control on multiphase flow in fractures and provides a basis for developing a rigorous upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Plain Language Summary
Multiphase flow in fractured media is an important process involved in many natural processes and subsurface engineering applications. Geological fractures are inherently rough to various degrees. The roughness of rock fracture, inducing irregular flow passages, plays a fundamental role in the displacement of one fluid by another immiscible one. Despite its importance, how the roughness controls the displacement patterns remains poorly understood. Here, we propose a theoretical model to quantify the impact of displacement patterns, which describes the two transitions of displacement patterns from capillary fingering to the crossover to viscous fingering as functions of roughness. The phase diagram predicted by the theoretical model is in excellent agreement with our experimental results. We also find that higher roughness index λb causes more dissipated energy. The dissipation ratio, representing the percentage of dissipated energy to the external work, increases from 39% to 61% as λb increases from 0.082 to 0.245 in the capillary fingering regime. Our work proposes a phase diagram to elucidate the impact of roughness on multiphase flow that is previously not reported; it also provides a basis for an upscaling methodology that relates Darcy‐scale flow behavior to the local fluid displacements via energy dissipation.
Key Points
A theoretical model is proposed to describe the two transitions of displacement patterns in rock fractures as functions of roughness
The phase diagram predicted by the model agrees very well with experiments, showing a destabilizing effect of roughness on fronts
As roughness index increases, the ratio of dissipated energy to external work increases from 39% to 61% in the capillary fingering regime</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1029/2019GL084762</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0002-2296-050X</orcidid><orcidid>https://orcid.org/0000-0001-9104-4401</orcidid><orcidid>https://orcid.org/0000-0002-5685-0819</orcidid><orcidid>https://orcid.org/0000-0003-2328-7035</orcidid></addata></record> |
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source | Wiley-Blackwell AGU Digital Archive |
subjects | Displacement displacement pattern Energy dissipation Energy exchange Fractures Fronts Methods Multiphase flow phase diagram Phase diagrams Porous media rock fractures Rocks Roughness |
title | Roughness Control on Multiphase Flow in Rock Fractures |
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