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dc.contributor.authorShawky, Ahmed
dc.contributor.authorEl-Anbaawy, Mohamed Ibrahim
dc.contributor.authorSoliman, Reham
dc.contributor.authorShaheen, Eslam Nasr
dc.contributor.authorOsman, Osama Abdelaziz
dc.contributor.authorHafiez, Hesham Eid Abdel
dc.contributor.authorShallaly, Nahla Ahmed
dc.date.accessioned2025-01-08T10:07:49Z
dc.date.available2025-01-08T10:07:49Z
dc.date.issued2024
dc.identifier.citationScience of The Total Environment, octubre 2024, vol. 946, 174283es
dc.identifier.issn0048-9697es
dc.identifier.urihttps://uvadoc.uva.es/handle/10324/73132
dc.descriptionProducción Científicaes
dc.description.abstractHammam Faraun (HF) geothermal site in Egypt shows potential for addressing energy demand and fossil fuel shortages. This study utilizes abandoned oil well logs, seismic data, and surface geology to assess HF geothermal energy resources. Seismic interpretation identified a significant clysmic fault parallel to Hammam Faraun fault (HFF), named CLB fault. The two faults together create a renewable geothermal cycle through circulation of mixed formation-sea waters. Petrophysics revealed two main geothermal reservoirs: the Nubian sandstone reservoir and the Eocene Thebes carbonate reservoir with water saturation values approaching 100 %. Corrected borehole temperatures indicated reservoir temperatures around 120 °C and 140 °C for the Thebes and Nubian reservoirs, respectively. Fracture analysis and stress state provided insights into subsurface fractures. A geomechanical model demonstrated the impact of different stresses and pore pressure on geothermal fluid flow. NE-SW oriented fractures showed a higher dilation tendency due to aquathermal expansion. The integrated conceptual geothermal model suggested a magma chamber beneath HF as the heat source, related to Oligo-Miocene volcanic activity. The breached relay ramp and fault-related open fracture system serve as pathways for geothermal fluids. Evaluation of the geothermal potential utilized volumetric calculations and Monte Carlo simulation. The estimated hot water volumes were 1.72 km3, 4.242 km3, and 5.332 km3 for the Nubian reservoir in the onshore part, Thebes reservoir in the offshore part, and Nubian reservoir in the offshore part, respectively. The results indicate a medium enthalpy resource suitable for electricity generation using a Kalina geothermal power plant. The predicted geothermal power output is promising, with an average power output of 9.64 MWe, 21.38 MWe, and 43.76 MWe for the Nubian reservoir in the onshore part, Thebes reservoir in the offshore part, and Nubian reservoir in the offshore part, respectively. These outputs can potentially supply electricity to approximately 12,000, 29,000 and 53,000 households, respectively.es
dc.format.mimetypeapplication/pdfes
dc.language.isoenges
dc.publisherElsevieres
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subject.classificationGeothermal energyes
dc.subject.classificationRiftes
dc.subject.classificationHammam Faraun (HF)es
dc.subject.classificationGeomechanical modeles
dc.subject.classificationDilation tendencyes
dc.subject.classificationMagma chamberes
dc.subject.classificationMonte Carlo simulationes
dc.titleUtilization of abandoned oil well logs and seismic data for modeling and assessing deep geothermal energy resources: A case studyes
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© 2024 The Authorses
dc.identifier.doi10.1016/j.scitotenv.2024.174283es
dc.relation.publisherversionhttps://www.sciencedirect.com/science/article/pii/S0048969724044310es
dc.identifier.publicationfirstpage174283es
dc.identifier.publicationtitleScience of The Total Environmentes
dc.identifier.publicationvolume946es
dc.peerreviewedSIes
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones
dc.subject.unesco3322.05 Fuentes no Convencionales de Energíaes


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