A finite volume method for advection-diffusion problems in convection-dominated regimes (Articolo in rivista)

Type
Label
  • A finite volume method for advection-diffusion problems in convection-dominated regimes (Articolo in rivista) (literal)
Anno
  • 2008-01-01T00:00:00+01:00 (literal)
Alternative label
  • Manzini G., Russo A. (2008)
    A finite volume method for advection-diffusion problems in convection-dominated regimes
    in Computer methods in applied mechanics and engineering
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Manzini G., Russo A. (literal)
Pagina inizio
  • 1242 (literal)
Pagina fine
  • 1261 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 197 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 13-16 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • IMATI-CNR Universita di Milano Bicocca, Milano (literal)
Titolo
  • A finite volume method for advection-diffusion problems in convection-dominated regimes (literal)
Abstract
  • We present a finite volume method for the numerical approximation of advection diffusion problems in convection-dominated regimes. The method works on unstructured grids formed by convex polygons of any shape and yields a piecewise linear approximation to the exact solution which is second-order accurate away from boundary and internal layers. Basically, we define a constant approximation of the solution gradient in every mesh cell which is expressed by using the cell averages of the solution within the adjacent cells. A careful design of the reconstruction algorithm for cell gradients and the introduction in the discrete formulation of a special non-linear term, which plays the role of the artificial diffusion, allows the method to achieve shock-capturing capability. We emphasize that no slope limiters are required by this approach. Optimal convergence rates, as theoretically expected, and non-oscillatory behavior close to layers are confirmed by numerical experiments. (literal)
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