3D groundwater flow and deformation modelling of Madrid aquifer

Por favor, use este identificador para citar o enlazar este ítem: http://hdl.handle.net/10045/103419
Registro completo de metadatos
Registro completo de metadatos
Campo DCValorIdioma
dc.contributorIngeniería del Terreno y sus Estructuras (InTerEs)es_ES
dc.contributor.authorBonì, Roberta-
dc.contributor.authorMeisina, Claudia-
dc.contributor.authorTeatini, Pietro-
dc.contributor.authorZucca, Francesco-
dc.contributor.authorZoccarato, Claudia-
dc.contributor.authorFranceschini, Andrea-
dc.contributor.authorEzquerro Martín, Pablo-
dc.contributor.authorBéjar Pizarro, Marta-
dc.contributor.authorFernández-Merodo, José Antonio-
dc.contributor.authorGuardiola-Albert, Carolina-
dc.contributor.authorPastor Navarro, José Luis-
dc.contributor.authorTomás, Roberto-
dc.contributor.authorHerrera García, Gerardo-
dc.contributor.otherUniversidad de Alicante. Departamento de Ingeniería Civiles_ES
dc.date.accessioned2020-03-03T12:52:16Z-
dc.date.available2020-03-03T12:52:16Z-
dc.date.issued2020-02-28-
dc.identifier.citationJournal of Hydrology. 2020, 585: 124773. doi:10.1016/j.jhydrol.2020.124773es_ES
dc.identifier.issn0022-1694 (Print)-
dc.identifier.issn1879-2707 (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/103419-
dc.description.abstractA novel methodological approach to calibrate and validate three-dimensional (3D) finite element (FE) groundwater flow and geomechanical models has been implemented using Advanced Differential Interferometric SAR (A-DInSAR) data. In particular, we show how A-DInSAR data can be effectively used to (1) constrain the model set-up in evaluating the areal influence of the wellfield and (2) characterise the aquifer system, specifically the storage coefficient values, which represents a fundamental step in managing groundwater resources. The procedure has been tested to reconstruct the surface vertical and horizontal movements caused by the Manzanares-Jarama wellfield located northwest of Madrid (Spain). The wellfield was used to supply freshwater during major droughts over the period between 1994 and 2010. Previous A-DInSAR outcomes obtained by ERS-1/2 and ENVISAT acquisitions clearly revealed the seasonality of the land displacements associated to the withdrawal and recovery cycles that characterized the wellfield development. A time-lag of about one month, which is in the order of the time span between two SAR acquisitions, between the hydraulic head changes and the displacements has been detected in this site by a wavelet analysis of A-DInSAR and piezometer time series. The negligible delay between the forcing factor and the system response and the complete subsidence recovery when piezometric head recovers supported the understanding of a minor role played by the pore pressure propagation within clay layers and the almost perfectly elastic behavior of the system (viscosity is negligible), respectively. The developed geomechanical model satisfactorily reproduces the pumping-induced deformations with a Root Mean Square Error (RMSE) between observed and simulated land displacements in the order of 0.1-0.3 mm. The results give insights about the approach benefits in deeply understanding the spatio-temporal aquifer-system response to the management of this strategic water resource for Madrid.es_ES
dc.description.sponsorshipThe activity has been developed within the scientific collaboration established in the framework of the UNESCO Land Subsidence International Initiative (LaSII - https://www.landsubsidence-unesco.org/). The research was funded by University of Pavia in the framework of a research grant award “assegno di tipo A premiale” for research activities at the Dept. of Earth and Environmental Sciences, within the research project entitled “Sustainable groundwater resources management by integrating A-DInSAR derived monitoring and flow modeling results” assigned to Roberta Bonì in March 2019. This research was partially funded by the Spanish Ministry of Economy, Industry and Competitiveness (MINECO), the State Agency of Research (AEI), and the European Funds for Regional Development (FEDER) under project TEC2017-85244-C2-1-P.es_ES
dc.languageenges_ES
dc.publisherElsevieres_ES
dc.rights© 2020 Published by Elsevier B.V.es_ES
dc.subjectSeasonal deformationes_ES
dc.subjectLand subsidencees_ES
dc.subject3D Finite Element (FE) groundwater and geomechanical modeles_ES
dc.subjectA-DInSAR techniquees_ES
dc.subjectGroundwater managementes_ES
dc.subject.otherIngeniería del Terrenoes_ES
dc.title3D groundwater flow and deformation modelling of Madrid aquiferes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.peerreviewedsies_ES
dc.identifier.doi10.1016/j.jhydrol.2020.124773-
dc.relation.publisherversionhttps://doi.org/10.1016/j.jhydrol.2020.124773es_ES
dc.identifier.cvIDA10235840-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/TEC2017-85244-C2-1-P-
Aparece en las colecciones:INV - INTERES - Artículos de Revistas

Archivos en este ítem:
Archivos en este ítem:
Archivo Descripción TamañoFormato 
Thumbnail2020_Boni_etal_JHydrology_preprint.pdfPreprint (acceso abierto)6,48 MBAdobe PDFAbrir Vista previa
Thumbnail2020_Boni_etal_JHydrology_final.pdfVersión final (acceso restringido)33,33 MBAdobe PDFAbrir    Solicitar una copia


Todos los documentos en RUA están protegidos por derechos de autor. Algunos derechos reservados.