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dc.contributor.authorChamekh, Khemissi-
dc.contributor.authorDjaballah, Brahim-
dc.contributor.authorBenkhedda, Abdelhakim-
dc.contributor.authorDjemmal, Samir-
dc.date.accessioned2020-12-21T00:44:03Z-
dc.date.available2020-12-21T00:44:03Z-
dc.date.issued2019-10-15-
dc.identifier.urihttp://dspace.univ-ouargla.dz/jspui/handle/123456789/24471-
dc.descriptionSéminaire International sur l′Hydrogéologie et l′Environnement SIHE 2019 Ouarglaen_US
dc.description.abstractThe main goal of this study is to analyze the surface part of the karst and some underground characteristics of Eocene karst system.The Karst cavities are widespread in the Eocene forming the upper formation under the Quaternary cover in the Cheria syncline. The Eocene limestone aquifer is intensively fractured and karstified. Major sub surface karst cavities is located nourthen and centre part of Cheria syncline.Hence, cavity roof thickness are varied with geometrical and geomchanical parameters on the fractured rock. The depth of the karstified zones depends on the geomechanical parameters, which is controlled by the fracture aperture distribution (Renshaw. DOI: 10.1029/ 95 JB 02159. ISSN: 0148-0227.1995)...en_US
dc.publisherUniversité Kasdi Merbah Ouarglaen_US
dc.subjectFracturesen_US
dc.subjectKarsten_US
dc.subjectCavitiesen_US
dc.subjectSimulationen_US
dc.subjectCheriaen_US
dc.subjectAlgeriaen_US
dc.titleInfluence of geomechanical and hydraulic parameters of the fractured rock on the evolution of underground karst cavities in Cheria area, NE Algereaen_US
dc.typeArticleen_US
Appears in Collections:4. Faculté des Hydrocarbures, des Energies Renouvelables, des Sciences de la Terre et de l’Univers

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