Porous medium coffee ring effect and other factors affecting the first crystallisation time of sodium chloride at the surface of a drying porous medium
We study the distribution of ions in a drying porous medium up to the formation of first crystals at the surface. The study is based on comparisons between numerical simulations and experiments with packings of glass beads. The experimental configuration, which is representative of many previous dry...
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Veröffentlicht in: | Physics of fluids (1994) 2013-12, Vol.25 (12) |
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creator | Hidri, F Sghaier, N Eloukabi, H Prat, M Nasrallah, SBen |
description | We study the distribution of ions in a drying porous medium up to the formation of first crystals at the surface. The study is based on comparisons between numerical simulations and experiments with packings of glass beads. The experimental configuration, which is representative of many previous drying experiments, is characterized by the formation of an efflorescence fairy ring at the surface of the porous medium. The preferential formation of crystals at the periphery is explained by the combined effect of higher evaporation fluxes at the surface periphery, as in the classical coffee ring problem, and variations in the porosity near the wall bordering the packing. It is shown that both effects have a great impact on the time marking the occurrence of first crystals, which is referred to as the first crystallization time. The experiments indicate that the first crystallization time increases with a decreasing bead size for a given initial ion concentration. This is explained by the variation with bead size of the characteristic size of the near wall region where a preferential desaturation of the sample occurs as a result of the porosity increase near the wall. The study also reveals a significant salt supersaturation effect. This represents a noticeable fact in relation with salt weathering issues. |
doi_str_mv | 10.1063/1.4834356 |
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The study is based on comparisons between numerical simulations and experiments with packings of glass beads. The experimental configuration, which is representative of many previous drying experiments, is characterized by the formation of an efflorescence fairy ring at the surface of the porous medium. The preferential formation of crystals at the periphery is explained by the combined effect of higher evaporation fluxes at the surface periphery, as in the classical coffee ring problem, and variations in the porosity near the wall bordering the packing. It is shown that both effects have a great impact on the time marking the occurrence of first crystals, which is referred to as the first crystallization time. The experiments indicate that the first crystallization time increases with a decreasing bead size for a given initial ion concentration. This is explained by the variation with bead size of the characteristic size of the near wall region where a preferential desaturation of the sample occurs as a result of the porosity increase near the wall. The study also reveals a significant salt supersaturation effect. 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The study is based on comparisons between numerical simulations and experiments with packings of glass beads. The experimental configuration, which is representative of many previous drying experiments, is characterized by the formation of an efflorescence fairy ring at the surface of the porous medium. The preferential formation of crystals at the periphery is explained by the combined effect of higher evaporation fluxes at the surface periphery, as in the classical coffee ring problem, and variations in the porosity near the wall bordering the packing. It is shown that both effects have a great impact on the time marking the occurrence of first crystals, which is referred to as the first crystallization time. The experiments indicate that the first crystallization time increases with a decreasing bead size for a given initial ion concentration. This is explained by the variation with bead size of the characteristic size of the near wall region where a preferential desaturation of the sample occurs as a result of the porosity increase near the wall. The study also reveals a significant salt supersaturation effect. This represents a noticeable fact in relation with salt weathering issues.</description><subject>Beads</subject><subject>Coffee</subject><subject>Computer simulation</subject><subject>Crystallization</subject><subject>Crystals</subject><subject>Desaturation</subject><subject>Drying</subject><subject>Efflorescence</subject><subject>Engineering Sciences</subject><subject>Experiments</subject><subject>Fluid dynamics</subject><subject>Fluid mechanics</subject><subject>Fluids mechanics</subject><subject>Fluxes</subject><subject>Formations</subject><subject>Ion concentration</subject><subject>Mathematical analysis</subject><subject>Mathematical models</subject><subject>Mechanics</subject><subject>Physics</subject><subject>Porosity</subject><subject>Porous media</subject><subject>Sodium chloride</subject><subject>Supersaturation</subject><subject>Walls</subject><subject>Weathering</subject><issn>1070-6631</issn><issn>0031-9171</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkctKLDEQhhs5gteFbxBwo4vWSieddC9FvMGALnQd0rk4ke7OmKQPzJP4uqZnxCNuzipF1Zefr6iiOMFwgYGRS3xBG0JJzXaKfQxNW3LG2J-55lAyRvBecRDjGwCQtmL7xceTD36KaDDaTQNS3lpjUHDjKzK5VAnJUSOfliYgK1XyISK5GcxIbiPrQkxIhXVMsu9dlMn5ESU3GOQtin6bu-x9cNogmTaf4hRy2oaQSIf1HLb6aXJU7FrZR3P89R4WL7c3z9f35eLx7uH6alGq7J9KXEkJNae6NpJAoyl0umGdpV3VtUQpClRZiquO1xQ4JpxVLbVaGa3y2HbksDjf5i5lL1bBDTKshZdO3F8txNwDaOsKKP-LM3u2ZVfBv08mJjG4qEzfy9Fkc4E5BwKck-b_aM04zuIMMnr6C33zUxjz0qLCFeeshZr981TBxxiM_ZbFIObLCyy-Lk8-AUf2oMc</recordid><startdate>20131201</startdate><enddate>20131201</enddate><creator>Hidri, F</creator><creator>Sghaier, N</creator><creator>Eloukabi, H</creator><creator>Prat, M</creator><creator>Nasrallah, SBen</creator><general>American Institute of Physics</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7U5</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-8685-6595</orcidid></search><sort><creationdate>20131201</creationdate><title>Porous medium coffee ring effect and other factors affecting the first crystallisation time of sodium chloride at the surface of a drying porous medium</title><author>Hidri, F ; Sghaier, N ; Eloukabi, H ; Prat, M ; Nasrallah, SBen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c392t-12aa0574d5ea308d40bd86bf4b2b93cc404cf412b754071376294fdcedc93cfb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Beads</topic><topic>Coffee</topic><topic>Computer simulation</topic><topic>Crystallization</topic><topic>Crystals</topic><topic>Desaturation</topic><topic>Drying</topic><topic>Efflorescence</topic><topic>Engineering Sciences</topic><topic>Experiments</topic><topic>Fluid dynamics</topic><topic>Fluid mechanics</topic><topic>Fluids mechanics</topic><topic>Fluxes</topic><topic>Formations</topic><topic>Ion concentration</topic><topic>Mathematical analysis</topic><topic>Mathematical models</topic><topic>Mechanics</topic><topic>Physics</topic><topic>Porosity</topic><topic>Porous media</topic><topic>Sodium chloride</topic><topic>Supersaturation</topic><topic>Walls</topic><topic>Weathering</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hidri, F</creatorcontrib><creatorcontrib>Sghaier, N</creatorcontrib><creatorcontrib>Eloukabi, H</creatorcontrib><creatorcontrib>Prat, M</creatorcontrib><creatorcontrib>Nasrallah, SBen</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hidri, F</au><au>Sghaier, N</au><au>Eloukabi, H</au><au>Prat, M</au><au>Nasrallah, SBen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Porous medium coffee ring effect and other factors affecting the first crystallisation time of sodium chloride at the surface of a drying porous medium</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2013-12-01</date><risdate>2013</risdate><volume>25</volume><issue>12</issue><issn>1070-6631</issn><issn>0031-9171</issn><eissn>1089-7666</eissn><abstract>We study the distribution of ions in a drying porous medium up to the formation of first crystals at the surface. The study is based on comparisons between numerical simulations and experiments with packings of glass beads. The experimental configuration, which is representative of many previous drying experiments, is characterized by the formation of an efflorescence fairy ring at the surface of the porous medium. The preferential formation of crystals at the periphery is explained by the combined effect of higher evaporation fluxes at the surface periphery, as in the classical coffee ring problem, and variations in the porosity near the wall bordering the packing. It is shown that both effects have a great impact on the time marking the occurrence of first crystals, which is referred to as the first crystallization time. The experiments indicate that the first crystallization time increases with a decreasing bead size for a given initial ion concentration. This is explained by the variation with bead size of the characteristic size of the near wall region where a preferential desaturation of the sample occurs as a result of the porosity increase near the wall. The study also reveals a significant salt supersaturation effect. This represents a noticeable fact in relation with salt weathering issues.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/1.4834356</doi><orcidid>https://orcid.org/0000-0001-8685-6595</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Beads Coffee Computer simulation Crystallization Crystals Desaturation Drying Efflorescence Engineering Sciences Experiments Fluid dynamics Fluid mechanics Fluids mechanics Fluxes Formations Ion concentration Mathematical analysis Mathematical models Mechanics Physics Porosity Porous media Sodium chloride Supersaturation Walls Weathering |
title | Porous medium coffee ring effect and other factors affecting the first crystallisation time of sodium chloride at the surface of a drying porous medium |
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