Geomechanical modeling to assess the injection-induced fracture slip-potential and subsurface stability of the Cambro-Ordovician reservoirs of Hassi Terfa field, Algeria

dc.contributor.authorBenayad, Soumya
dc.contributor.authorSen, Souvik
dc.contributor.authorBaouche, Rafik
dc.contributor.authorMitra, Sourav
dc.contributor.authorChaouchi, Rabah
dc.date.accessioned2024-06-12T10:09:36Z
dc.date.available2024-06-12T10:09:36Z
dc.date.issued2024
dc.description.abstractThe in-situ stress state and the distribution of the critically stressed fractures have significant implications on optimum wellbore placement, production enhancement, fluid injection, and induced seismicity which largely influence the reservoir management strategies. This study presents a comprehensive geomechanical modeling to infer the likelihood of shear slippage of the optimally oriented weak planes in response to water injection in the deep Paleozoic oil reservoirs from the Hassi Terfa field, central Algerian Sahara. The ‘B-quality’ compressive failures, i.e., breakouts from the acoustic image log indicate the maximum horizontal stress azimuth as N114°E. The inferred in-situ stress magnitudes indicate a strike-slip tectonic regime in the study area. The reservoir is generally tight (porosity <8 %, permeability <0.4 mD) due to extensive silica cementation, however pre-existing closed to partially open natural fractures of variable geometries are identified on cores, thin sections, and image logs. The stress-based slip assessment indicates that none of the fracture geometries is critically stressed and hydraulically conductive at the initial reservoir stress state. The onset of slip on the critically oriented vertical fractures can initiate at 1200 psi of fluid injection at the reservoir level of ∼3500 m. The E-W to EES-WWN oriented fractures, parallel to the maximum horizontal stress azimuth, have a higher likelihood of being critically stressed during injection and therefore can contribute to the permeability enhancement. We restrict the practical injection threshold at 3000 psi, which can create tensile failures on the shale caprocks. We infer that the NE-SW and NNE-SSW striking, steeply dipping fractures and regional faults being perpendicular or at high angles to the regional maximum horizontal stress azimuth, are the most stable ones and therefore, less likely to slip within the practical injection limit.en_US
dc.identifier.issn1365-1609
dc.identifier.urihttps://www.sciencedirect.com/science/article/abs/pii/S1365160924001400?via%3Dihub
dc.identifier.urihttps://doi.org/10.1016/j.ijrmms.2024.105775
dc.identifier.urihttps://dspace.univ-boumerdes.dz/handle/123456789/14137
dc.language.isoenen_US
dc.publisherElsevier Ltden_US
dc.relation.ispartofseriesInternational Journal of Rock Mechanics and Mining Sciences/ Vol. 178, Art. N°105775 (2024);
dc.subjectFluid injectionen_US
dc.subjectGeomechanical modelingen_US
dc.subjectIn-situ stressesen_US
dc.subjectNaturally fractured reservoirsen_US
dc.subjectReservoir stabilityen_US
dc.subjectSlip potentialen_US
dc.titleGeomechanical modeling to assess the injection-induced fracture slip-potential and subsurface stability of the Cambro-Ordovician reservoirs of Hassi Terfa field, Algeriaen_US
dc.typeArticleen_US

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