Numerical simulation of natural convection using unsteady compressible Navier-stokes equations

Mahmoud M. El-Gendi, Abdelraheem M. Aly

Research output: Contribution to journalArticlepeer-review

10 Citations (Scopus)

Abstract

Purpose - Boussinesq approximation is widely used in solving natural convection problems, but it has severe practical limitations. Using Boussinesq approximation, the temperature difference should be less than 28.6 K. The purpose of this study is to get rid of Boussinesq approximation and simulates the natural convection problems using an unsteady compressible Navier-Stokes solver. The gravity force is included in the source term. Three temperature differences are used namely 20 K, 700 K and 2000 K. Design/methodology/approach - The calculations are carried out on the square and sinusoidal cavities. The results of low temperature difference have good agreement with the experimental and previous calculated data. It is found that, the high temperature difference has a significant effect on the density. Findings - Due to mass conservation, the density variation affects the velocity distribution and its symmetry. On the other hand, the density variation has a negligible effect on the temperature distribution. Originality/value - The present calculation method has no limitations but its convergence is slow. The current study can be used in fluid flow simulations for nuclear power applications in natural convection flows subjected to large temperature differences.

Original languageEnglish
Pages (from-to)2508-2527
Number of pages20
JournalInternational Journal of Numerical Methods for Heat and Fluid Flow
Volume27
Issue number11
DOIs
Publication statusPublished - 2017
Externally publishedYes

Keywords

  • Boussinesq approximation
  • Compressible solver
  • Natural convection
  • Navier-Stokes

ASJC Scopus subject areas

  • Mechanics of Materials
  • Mechanical Engineering
  • Computer Science Applications
  • Applied Mathematics

Fingerprint

Dive into the research topics of 'Numerical simulation of natural convection using unsteady compressible Navier-stokes equations'. Together they form a unique fingerprint.

Cite this