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Three-dimensional numerical study of natural convection in an inclined porous cavity with time sinusoidal oscillating boundary conditions

  • Xi'an Jiaotong University

Research output: Contribution to journalArticlepeer-review

35 Scopus citations

Abstract

Three-dimensional unsteady natural convections in an inclined porous cavity with time oscillating boundary conditions are numerically studied in this paper. The Darcy-Forchheimer-Brinkman model is adopted to model the fluid flow in the porous medium and the combination effects of inclination angles (α1, α2) and temperature oscillation frequency (f) on the convection characteristics with different Rayleigh numbers (Ra = 106 and 107) are carefully investigated, especially when the porous cavity is seriously inclined (80 ° ≤ α1 ≤ 90 °). It is revealed that, when the porous cavity is moderately inclined (0 ° ≤ α1 ≤ 75 °, α2 = 0 °), the natural convections inside are stable and quasi two-dimensional. However, if the cavity is seriously inclined (75 ° ≤ α1 ≤ 90 °, α2 = 0 °), the flow patterns inside are much more complicated and the three-dimensional multiple roll-cells with different intercrossing angles are established. It is also found that, when the porous cavity is inclined with three-dimensional method (α1 > 0°, α2 > 0°), the natural convections become quite different and a series of three-dimensional screw type flexural roll-cells appears. Furthermore, it is suggested that, with proper selection of inclination angles and oscillation frequency, the natural convection heat transfer will be significantly improved and the maximal heat fluxes are finally obtained at the optimal combinations of f = 35π, α1 = 50°, α2 = 45° when Ra = 106 and f = 40π, α1 = 45°, α2 = 45° when Ra = 107.

Original languageEnglish
Pages (from-to)70-82
Number of pages13
JournalInternational Journal of Heat and Fluid Flow
Volume31
Issue number1
DOIs
StatePublished - Feb 2010

Keywords

  • Inclined porous cavity
  • Natural convection
  • Numerical simulation
  • Temperature oscillation

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