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dc.contributor.authorGran Esforzado, Meritxell
dc.contributor.authorCarrera Ramírez, Jesús
dc.contributor.authorOlivella Pastallé, Sebastià
dc.contributor.authorSaaltink, Maarten Willem
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria del Terreny, Cartogràfica i Geofísica
dc.date.accessioned2011-03-08T18:41:08Z
dc.date.available2011-03-08T18:41:08Z
dc.date.created2011
dc.date.issued2011
dc.identifier.citationGran Esforzado, M. [et al.]. Modeling evaporation processes in a saline soil from saturation to oven dry conditions. "Hydrology and Earth system sciences discussions", 2011, vol. 8, núm. 1, p. 529-554.
dc.identifier.issn1812-2108
dc.identifier.urihttp://hdl.handle.net/2117/11733
dc.description.abstractThermal, suction and osmotic gradients interact during evaporation from a salty soil. Vapor fluxes become the main water flow mechanism under very dry conditions. A coupled nonisothermal multiphase flow and a reactive transport model of a salty sand soil was developed to study such an intricate system. The model was calibrated with data from an evaporation experiment (volumetric water content, temperature and concentration). The retention curve and relative permeability functions were modified to simulate oven dry conditions. Experimental observations were satisfactorily reproduced, which suggests that the model can be used to assess the underlying processes. Results show that evaporation is controlled by heat, and limited by salinity and liquid and vapor fluxes. Below evaporation front vapor flows downwards controlled by temperature gradient and thus generates a dilution. Vapor diffusion and dilution are strongly influenced by heat boundary conditions. Gas diffusion plays a major role in the magnitude of vapor fluxes.
dc.format.extent26 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Hidrologia subterrània
dc.subject.lcshReservoirs--Evaporation control
dc.subject.lcshEvaporation control
dc.titleModeling evaporation processes in a saline soil from saturation to oven dry conditions
dc.typeArticle
dc.subject.lemacEvaporació
dc.contributor.groupUniversitat Politècnica de Catalunya. GHS - Grup d'Hidrologia Subterrània
dc.contributor.groupUniversitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
dc.identifier.doi10.5194/hessd-8-529-2011
dc.relation.publisherversionhttp://www.hydrol-earth-syst-sci-discuss.net/8/529/2011/hessd-8-529-2011.html
dc.rights.accessOpen Access
local.identifier.drac4959529
dc.description.versionPostprint (published version)
local.citation.authorGran Esforzado, M.; Carrera, J.; Olivella, S.; Saaltink, M.
local.citation.publicationNameHydrology and Earth system sciences discussions
local.citation.volume8
local.citation.number1
local.citation.startingPage529
local.citation.endingPage554


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