Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/927
DC FieldValueLanguage
dc.contributor.advisorCabrera, M.C.es
dc.contributor.advisorHeredia, Javieres
dc.contributor.authorCruz-Fuentes, Tatianaen_US
dc.date.accessioned2009-10-08T02:31:00Z-
dc.date.accessioned2018-02-21T14:22:00Z-
dc.date.available2018-02-21T14:22:00Z-
dc.date.issued2007en_US
dc.identifier.isbn8799899529724en_US
dc.identifier.other2069-
dc.identifier.urihttp://hdl.handle.net/10553/927-
dc.description.abstractIn this study, a groundwater flow model of this aquifer is developed. The model simulates an average steadystate condition for the year 1992, when an extensive field study was undertaken, in which 238 wells were visited in the study area. The model simulates groundwater flow over an area of about 44 km2 with 190 rows, 201 columns and three layers. Based on the modelling results, the model reproduces the observed flow–field and the water balance components rather well. The model presents numeric stability problems due to the steep topography of the area that constitutes a determining factor.en_US
dc.languageengen_US
dc.sourceGroundwater and ecosystems. p. 1-9en_US
dc.subject.otherAgua subterráneaen_US
dc.subject.otherFlujoen_US
dc.subject.otherSimulaciónen_US
dc.subject.otherCanariasen_US
dc.subject.otherGran Canariaen_US
dc.subject.otherAcuífero volcánicoen_US
dc.titleSteady-state three-dimensional flow simulation in a volcanic-sedimentary aquiferen_US
dc.typeinfo:eu-repo/semantics/bookParten_US
dc.typeBookPartes
dc.contributor.authorscopusidCabrera, M.C.-
dc.contributor.authorscopusidHeredia, Javier-
dc.identifier.absysnet560566-
dc.identifier.crisid--
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.type2Capítulo de libroen_US
dc.identifier.external--
dc.identifier.ulpgces
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.fullNameCruz Fuentes, Tatiana-
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