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NSM analysis of time-dependent nonlinear buoyancy-driven double-diffusive radiative convection flow in non-Darcy geological porous media

  • O. A. Bég
  • , J. Zueco
  • , T. A. Bég
  • , H. S. Takhar
  • , E. Kahya
  • BAE Systems
  • Castle College
  • Technical University of Cartagena
  • Engineering Mechanics and Seismic Dynamics Research
  • Manchester Metropolitan University

Araştırma sonucu: Dergiye katkıMakalebilirkişi

36 Atıf (Scopus)

Özet

A network numerical simulator is developed and described to simulate the transient, nonlinear buoyancy-driven double diffusive heat and mass transfer of a viscous, incompressible, gray, absorbing-emitting fluid flowing past an impulsively started moving vertical plate adjacent to a non-Darcian geological porous regime. The governing boundary-layer equations are formulated in an (X *, Y *, t *) coordinate system with appropriate boundary conditions. An algebraic diffusion approximation is used to simplify the radiation heat transfer contribution. The non-dimensionalized transport equations are solved in an (X, Y, t) coordinate system using the network simulation model (NSM) and the computer code, Pspice. A detailed discussion of the network design is provided. The effects of Prandtl number, radiation-conduction parameter (Stark number), thermal Grashof number, species Grashof number, Schmidt number, Darcy number and Forchheimer number on the transient dimensionless velocities (U, V), non-dimensional temperature (T) and dimensionless concentration function (C) are illustrated graphically. Additionally, we have computed plots of U, V, T, C versus time and average Nusselt number and Sherwood number versus X, Y coordinate, for various thermophysical parameters. The model finds applications in geological contamination, geothermal energy systems and radioactive waste-repository near-field thermo-geofluid mechanics.

Orijinal dilİngilizce
Sayfa (başlangıç-bitiş)181-204
Sayfa sayısı24
DergiActa Mechanica
Hacim202
Basın numarası1-4
DOI'lar
Yayın durumuYayınlandı - Oca 2009

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