Matches in SemOpenAlex for { <https://semopenalex.org/work/W2122435865> ?p ?o ?g. }
- W2122435865 endingPage "367" @default.
- W2122435865 startingPage "355" @default.
- W2122435865 abstract "During high porosity reservoir production, the rock compaction is a complex phenomenon that depends on the rock constitutive behavior, the reservoir stress path, etc. Reservoir compaction can hardly be analyzed with conventional reservoir simulators as the pore compressibility factor, the only mechanical parameter used in such simulators, is not sufficient to represent the complex phenomena involved. In order to solve correctly this problem, the full thermohydro- mechanical equations must be addressed. The corresponding set of equations can be either solved simultaneously (fully coupled scheme) or using a conventional reservoir simulator in conjunction with a geomechanical simulator and information exchanges between the two simulators (partial coupling). The paper presents three formulations of the partial coupling, which are obtained in the framework of single-phase flow and a linear elastic isotropic rock behavior. This simple framework makes possible an easy and rigorous derivation of the porosity correction to be appended to the reservoir Lagrange's porosity used in the reservoir simulator. The porosity correction depends on the pore compressibility factor and a mechanical contribution that can be expressed either in terms of volumetric strain, pore volume change, or the mean total stress change. One formulation is tested on a numerical test that depicts the water flood through a laboratory core sample initially saturated with oil and constrained to uniaxial strain. The numerical test illustrates the importance of the mechanical effects on the fluid flow problem and validates the partial coupling proposed. The example also highlights the role of the pore compressibility factor in the partially coupled reservoir simulation. Actually, in the partially (iteratively) coupled approach, the pore compressibility factor can be interpreted as a relaxation parameter controlling the convergence speed of the iterative process between reservoir simulation and geomechanical simulation." @default.
- W2122435865 created "2016-06-24" @default.
- W2122435865 creator A5052672775 @default.
- W2122435865 creator A5082429977 @default.
- W2122435865 date "2002-07-01" @default.
- W2122435865 modified "2023-09-25" @default.
- W2122435865 title "Coupling Fluid Flow and Rock Mechanics: Formulations of the Partial Coupling Between Reservoir and Geomechanical Simulators" @default.
- W2122435865 cites W1999448485 @default.
- W2122435865 cites W2012746049 @default.
- W2122435865 cites W2028740696 @default.
- W2122435865 cites W2037661031 @default.
- W2122435865 cites W2050092501 @default.
- W2122435865 cites W2058371298 @default.
- W2122435865 cites W2080905548 @default.
- W2122435865 cites W2121872808 @default.
- W2122435865 cites W2180328610 @default.
- W2122435865 cites W2075768534 @default.
- W2122435865 doi "https://doi.org/10.2516/ogst:2002023" @default.
- W2122435865 hasPublicationYear "2002" @default.
- W2122435865 type Work @default.
- W2122435865 sameAs 2122435865 @default.
- W2122435865 citedByCount "80" @default.
- W2122435865 countsByYear W21224358652012 @default.
- W2122435865 countsByYear W21224358652013 @default.
- W2122435865 countsByYear W21224358652014 @default.
- W2122435865 countsByYear W21224358652015 @default.
- W2122435865 countsByYear W21224358652016 @default.
- W2122435865 countsByYear W21224358652017 @default.
- W2122435865 countsByYear W21224358652018 @default.
- W2122435865 countsByYear W21224358652019 @default.
- W2122435865 countsByYear W21224358652020 @default.
- W2122435865 countsByYear W21224358652021 @default.
- W2122435865 countsByYear W21224358652022 @default.
- W2122435865 countsByYear W21224358652023 @default.
- W2122435865 crossrefType "journal-article" @default.
- W2122435865 hasAuthorship W2122435865A5052672775 @default.
- W2122435865 hasAuthorship W2122435865A5082429977 @default.
- W2122435865 hasBestOaLocation W21224358651 @default.
- W2122435865 hasConcept C102579867 @default.
- W2122435865 hasConcept C105569014 @default.
- W2122435865 hasConcept C121332964 @default.
- W2122435865 hasConcept C127313418 @default.
- W2122435865 hasConcept C127413603 @default.
- W2122435865 hasConcept C131584629 @default.
- W2122435865 hasConcept C151730666 @default.
- W2122435865 hasConcept C183250156 @default.
- W2122435865 hasConcept C184050105 @default.
- W2122435865 hasConcept C185715996 @default.
- W2122435865 hasConcept C187320778 @default.
- W2122435865 hasConcept C196715460 @default.
- W2122435865 hasConcept C38349280 @default.
- W2122435865 hasConcept C548895740 @default.
- W2122435865 hasConcept C57879066 @default.
- W2122435865 hasConcept C62520636 @default.
- W2122435865 hasConcept C6648577 @default.
- W2122435865 hasConcept C78519656 @default.
- W2122435865 hasConcept C84655787 @default.
- W2122435865 hasConcept C90278072 @default.
- W2122435865 hasConcept C97842125 @default.
- W2122435865 hasConceptScore W2122435865C102579867 @default.
- W2122435865 hasConceptScore W2122435865C105569014 @default.
- W2122435865 hasConceptScore W2122435865C121332964 @default.
- W2122435865 hasConceptScore W2122435865C127313418 @default.
- W2122435865 hasConceptScore W2122435865C127413603 @default.
- W2122435865 hasConceptScore W2122435865C131584629 @default.
- W2122435865 hasConceptScore W2122435865C151730666 @default.
- W2122435865 hasConceptScore W2122435865C183250156 @default.
- W2122435865 hasConceptScore W2122435865C184050105 @default.
- W2122435865 hasConceptScore W2122435865C185715996 @default.
- W2122435865 hasConceptScore W2122435865C187320778 @default.
- W2122435865 hasConceptScore W2122435865C196715460 @default.
- W2122435865 hasConceptScore W2122435865C38349280 @default.
- W2122435865 hasConceptScore W2122435865C548895740 @default.
- W2122435865 hasConceptScore W2122435865C57879066 @default.
- W2122435865 hasConceptScore W2122435865C62520636 @default.
- W2122435865 hasConceptScore W2122435865C6648577 @default.
- W2122435865 hasConceptScore W2122435865C78519656 @default.
- W2122435865 hasConceptScore W2122435865C84655787 @default.
- W2122435865 hasConceptScore W2122435865C90278072 @default.
- W2122435865 hasConceptScore W2122435865C97842125 @default.
- W2122435865 hasIssue "4" @default.
- W2122435865 hasLocation W21224358651 @default.
- W2122435865 hasLocation W21224358652 @default.
- W2122435865 hasLocation W21224358653 @default.
- W2122435865 hasLocation W21224358654 @default.
- W2122435865 hasOpenAccess W2122435865 @default.
- W2122435865 hasPrimaryLocation W21224358651 @default.
- W2122435865 hasRelatedWork W1574710162 @default.
- W2122435865 hasRelatedWork W1970614936 @default.
- W2122435865 hasRelatedWork W1999844787 @default.
- W2122435865 hasRelatedWork W2048804069 @default.
- W2122435865 hasRelatedWork W2118040115 @default.
- W2122435865 hasRelatedWork W2188285657 @default.
- W2122435865 hasRelatedWork W2357457410 @default.
- W2122435865 hasRelatedWork W2380363375 @default.
- W2122435865 hasRelatedWork W2757345591 @default.
- W2122435865 hasRelatedWork W2944754093 @default.
- W2122435865 hasVolume "57" @default.