FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094348483> ?p ?o ?g. }

• W2094348483 abstract "Abstract Anisotropy of hydraulic properties of subsurface geologic formations is an essential feature that has been established as a consequence of the different geologic processes that they undergo during the longer geologic time scale. With respect to petroleum reservoirs, in many cases, anisotropy plays significant role in dictating the direction of flow that becomes no longer dependent only on the pressure gradient direction but also on the principal directions of anisotropy. Furthermore, in complex systems involving the flow of multiphase fluids in which the gravity and the capillarity play an important role, anisotropy can also have important influences. Therefore, there has been great deal of motivation to consider anisotropy when solving the governing conservation laws numerically. Unfortunately, the two-point flux approximation of finite difference approach is not capable of handling full tensor permeability fields. Lately, however, it has been possible to adapt the multipoint flux approximation that can handle anisotropy to the framework of finite difference schemes. In multipoint flux approximation method, the stencil of approximation is more involved, i.e., it requires the involvement of 9-point stencil for the 2-D model and 27-point stencil for the 3-D model. This is apparently challenging and cumbersome when making the global system of equations. In this work, we apply the equation-type approach, which is the experimenting pressure field approach that enables the solution of the global problem breaks into the solution of multitude of local problems that significantly reduce the complexity without affecting the accuracy of numerical solution. This approach also leads in reducing the computational cost during the simulation. We have applied this technique to a variety of anisotropy scenarios of 3-D subsurface flow problems and the numerical results demonstrate that the experimenting pressure field technique fits very well with the multipoint flux approximation method. Furthermore, the numerical results explicitly emphasize that anisotropy could not be ignored for the proper model of subsurface flow." @default.
• W2094348483 created "2016-06-24" @default.
• W2094348483 creator A5014709706 @default.
• W2094348483 creator A5026966481 @default.
• W2094348483 creator A5057212913 @default.
• W2094348483 date "2013-09-16" @default.
• W2094348483 modified "2023-10-18" @default.
• W2094348483 title "3-D Numerical Investigation of Subsurface Flow in Anisotropic Porous Media using Multipoint Flux Approximation Method" @default.
• W2094348483 cites W1530030810 @default.
• W2094348483 cites W1545095299 @default.
• W2094348483 cites W1979431749 @default.
• W2094348483 cites W1995717402 @default.
• W2094348483 cites W2006976650 @default.
• W2094348483 cites W2017119616 @default.
• W2094348483 cites W2020862018 @default.
• W2094348483 cites W2034170310 @default.
• W2094348483 cites W2044943849 @default.
• W2094348483 cites W2064019732 @default.
• W2094348483 cites W2067276325 @default.
• W2094348483 cites W2081367955 @default.
• W2094348483 cites W2091443061 @default.
• W2094348483 cites W2127468063 @default.
• W2094348483 doi "https://doi.org/10.2118/165960-ms" @default.
• W2094348483 hasPublicationYear "2013" @default.
• W2094348483 type Work @default.
• W2094348483 sameAs 2094348483 @default.
• W2094348483 citedByCount "6" @default.
• W2094348483 countsByYear W20943484832014 @default.
• W2094348483 countsByYear W20943484832015 @default.
• W2094348483 countsByYear W20943484832016 @default.
• W2094348483 countsByYear W20943484832019 @default.
• W2094348483 crossrefType "proceedings-article" @default.
• W2094348483 hasAuthorship W2094348483A5014709706 @default.
• W2094348483 hasAuthorship W2094348483A5026966481 @default.
• W2094348483 hasAuthorship W2094348483A5057212913 @default.
• W2094348483 hasConcept C120665830 @default.
• W2094348483 hasConcept C121332964 @default.
• W2094348483 hasConcept C126255220 @default.
• W2094348483 hasConcept C134306372 @default.
• W2094348483 hasConcept C181330731 @default.
• W2094348483 hasConcept C191897082 @default.
• W2094348483 hasConcept C192562407 @default.
• W2094348483 hasConcept C28826006 @default.
• W2094348483 hasConcept C33923547 @default.
• W2094348483 hasConcept C38349280 @default.
• W2094348483 hasConcept C41008148 @default.
• W2094348483 hasConcept C459310 @default.
• W2094348483 hasConcept C57879066 @default.
• W2094348483 hasConcept C68709404 @default.
• W2094348483 hasConcept C76752949 @default.
• W2094348483 hasConcept C85725439 @default.
• W2094348483 hasConceptScore W2094348483C120665830 @default.
• W2094348483 hasConceptScore W2094348483C121332964 @default.
• W2094348483 hasConceptScore W2094348483C126255220 @default.
• W2094348483 hasConceptScore W2094348483C134306372 @default.
• W2094348483 hasConceptScore W2094348483C181330731 @default.
• W2094348483 hasConceptScore W2094348483C191897082 @default.
• W2094348483 hasConceptScore W2094348483C192562407 @default.
• W2094348483 hasConceptScore W2094348483C28826006 @default.
• W2094348483 hasConceptScore W2094348483C33923547 @default.
• W2094348483 hasConceptScore W2094348483C38349280 @default.
• W2094348483 hasConceptScore W2094348483C41008148 @default.
• W2094348483 hasConceptScore W2094348483C459310 @default.
• W2094348483 hasConceptScore W2094348483C57879066 @default.
• W2094348483 hasConceptScore W2094348483C68709404 @default.
• W2094348483 hasConceptScore W2094348483C76752949 @default.
• W2094348483 hasConceptScore W2094348483C85725439 @default.
• W2094348483 hasLocation W20943484831 @default.
• W2094348483 hasOpenAccess W2094348483 @default.
• W2094348483 hasPrimaryLocation W20943484831 @default.
• W2094348483 hasRelatedWork W1409194387 @default.
• W2094348483 hasRelatedWork W1858809761 @default.
• W2094348483 hasRelatedWork W1968203803 @default.
• W2094348483 hasRelatedWork W2013314297 @default.
• W2094348483 hasRelatedWork W2092925746 @default.
• W2094348483 hasRelatedWork W2387296223 @default.
• W2094348483 hasRelatedWork W2760830361 @default.
• W2094348483 hasRelatedWork W3011191910 @default.
• W2094348483 hasRelatedWork W4286800400 @default.
• W2094348483 hasRelatedWork W4302773302 @default.
• W2094348483 isParatext "false" @default.
• W2094348483 isRetracted "false" @default.
• W2094348483 magId "2094348483" @default.
• W2094348483 workType "article" @default.