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Morphology, propagation dynamics and scaling characteristics of drying fronts in porous media
Effects of surface wettability on the dynamics and morphology of evaporation‐induced drying fronts (DF) receding into hydrophilic (HI) or hydrophobic (HO) sands were studied using highly‐resolved neutron radiography. A more pronounced pinning‐depinning motion (larger steps and longer waiting times)...
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Published in: | Geophysical research letters 2012-05, Vol.39 (9), p.n/a |
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description | Effects of surface wettability on the dynamics and morphology of evaporation‐induced drying fronts (DF) receding into hydrophilic (HI) or hydrophobic (HO) sands were studied using highly‐resolved neutron radiography. A more pronounced pinning‐depinning motion (larger steps and longer waiting times) was observed for the DF in HI sand relative to HO, due to weaker capillary pinning forces in the latter. For length scalesl smaller than a correlation length ξ, quenched disorder dominates DF roughness expressed by a roughness exponent α = 0.77, whereas for l > ξ the fluctuations induced by the DF motion annealed the disorder and result in α= 0.44. Although wettability suppressed evaporation rates in HO relative to HI sand, differences in the evaporation dynamics and pinning behavior did not alter the DF morphology indicators‐the fractal dimension and roughness exponent‐which remained similar for the HI and HO sands.
Key Points
Hydrophobicity reduces velocity of DF displacement
Wettability weakly affects the fractal dimension and roughness exponent of DF
Lesser wettability limits the extent of film region and the evaporation rate |
doi_str_mv | 10.1029/2012GL051506 |
format | article |
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Key Points
Hydrophobicity reduces velocity of DF displacement
Wettability weakly affects the fractal dimension and roughness exponent of DF
Lesser wettability limits the extent of film region and the evaporation rate</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2012GL051506</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Drying ; Earth sciences ; Earth, ocean, space ; Evaporation ; Evaporation rate ; Exact sciences and technology ; fractal dimension ; Fractals ; Geophysics ; Hydrology ; liquid phase distribution ; Nonlinear systems ; Porous media ; Radiography ; roughness of drying front ; Sand ; wettability effects</subject><ispartof>Geophysical research letters, 2012-05, Vol.39 (9), p.n/a</ispartof><rights>Copyright 2012 by the American Geophysical Union</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4783-b5ce09f1f03e45bee1b7d306c69160ee6d4802dff44a0f8d8f03903a2e443e553</citedby><cites>FETCH-LOGICAL-c4783-b5ce09f1f03e45bee1b7d306c69160ee6d4802dff44a0f8d8f03903a2e443e553</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2012GL051506$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2012GL051506$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,11514,27924,27925,46468,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25968969$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Shokri, N.</creatorcontrib><creatorcontrib>Sahimi, Muhammad</creatorcontrib><creatorcontrib>Or, D.</creatorcontrib><title>Morphology, propagation dynamics and scaling characteristics of drying fronts in porous media</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Effects of surface wettability on the dynamics and morphology of evaporation‐induced drying fronts (DF) receding into hydrophilic (HI) or hydrophobic (HO) sands were studied using highly‐resolved neutron radiography. A more pronounced pinning‐depinning motion (larger steps and longer waiting times) was observed for the DF in HI sand relative to HO, due to weaker capillary pinning forces in the latter. For length scalesl smaller than a correlation length ξ, quenched disorder dominates DF roughness expressed by a roughness exponent α = 0.77, whereas for l > ξ the fluctuations induced by the DF motion annealed the disorder and result in α= 0.44. Although wettability suppressed evaporation rates in HO relative to HI sand, differences in the evaporation dynamics and pinning behavior did not alter the DF morphology indicators‐the fractal dimension and roughness exponent‐which remained similar for the HI and HO sands.
Key Points
Hydrophobicity reduces velocity of DF displacement
Wettability weakly affects the fractal dimension and roughness exponent of DF
Lesser wettability limits the extent of film region and the evaporation rate</description><subject>Drying</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Evaporation</subject><subject>Evaporation rate</subject><subject>Exact sciences and technology</subject><subject>fractal dimension</subject><subject>Fractals</subject><subject>Geophysics</subject><subject>Hydrology</subject><subject>liquid phase distribution</subject><subject>Nonlinear systems</subject><subject>Porous media</subject><subject>Radiography</subject><subject>roughness of drying front</subject><subject>Sand</subject><subject>wettability effects</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp9kEtPGzEUhS1UJALtrj_AEmLHtNfPGS8Rj7RqoBWlYoUsx2MHQzIe7Ilg_j2OghCrru6V7nfO1TkIfSXwjQBV3ykQOp2BIALkDpoQxXnVANSf0ARAlZ3Wcg_t5_wAAAwYmaC7y5j6-7iMi_EY9yn2ZmGGEDvcjp1ZBZux6VqcrVmGboHtvUnGDi6FPGxu0eM2jZuLT7EbMg4d7mOK64xXrg3mM9r1Zpndl7d5gP5dnN-c_qhmv6c_T09mleV1w6q5sA6UJx6Y42LuHJnXLQNppSISnJMtb4C23nNuwDdtU0AFzFDHOXNCsAN0uPUtCZ7WLg_6Ia5TV15qAoQJBo3khTreUjbFnJPzuk9hZdJYIL0pUH8ssOBHb6Zmk98n09mQ3zVUKNkoqQpHt9xzWLrxv556ej2jighWRNVWVJp0L-8ikx61rFkt9O3VVJ9d_uHi199b3bBXAvWN-w</recordid><startdate>201205</startdate><enddate>201205</enddate><creator>Shokri, N.</creator><creator>Sahimi, Muhammad</creator><creator>Or, D.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><general>John Wiley & Sons, Inc</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>201205</creationdate><title>Morphology, propagation dynamics and scaling characteristics of drying fronts in porous media</title><author>Shokri, N. ; 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Res. Lett</addtitle><date>2012-05</date><risdate>2012</risdate><volume>39</volume><issue>9</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Effects of surface wettability on the dynamics and morphology of evaporation‐induced drying fronts (DF) receding into hydrophilic (HI) or hydrophobic (HO) sands were studied using highly‐resolved neutron radiography. A more pronounced pinning‐depinning motion (larger steps and longer waiting times) was observed for the DF in HI sand relative to HO, due to weaker capillary pinning forces in the latter. For length scalesl smaller than a correlation length ξ, quenched disorder dominates DF roughness expressed by a roughness exponent α = 0.77, whereas for l > ξ the fluctuations induced by the DF motion annealed the disorder and result in α= 0.44. Although wettability suppressed evaporation rates in HO relative to HI sand, differences in the evaporation dynamics and pinning behavior did not alter the DF morphology indicators‐the fractal dimension and roughness exponent‐which remained similar for the HI and HO sands.
Key Points
Hydrophobicity reduces velocity of DF displacement
Wettability weakly affects the fractal dimension and roughness exponent of DF
Lesser wettability limits the extent of film region and the evaporation rate</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2012GL051506</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Drying Earth sciences Earth, ocean, space Evaporation Evaporation rate Exact sciences and technology fractal dimension Fractals Geophysics Hydrology liquid phase distribution Nonlinear systems Porous media Radiography roughness of drying front Sand wettability effects |
title | Morphology, propagation dynamics and scaling characteristics of drying fronts in porous media |
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