Skip to main content
Log in

Mixed convection in a porous medium produced by a line heat source

  • Published:
Transport in Porous Media Aims and scope Submit manuscript

Abstract

A boundary-layer analysis is presented for the mixed convection flow which is produced when a horizontal line heat source, which is embedded in an infinite fluid-saturated porous medium, generates heat at a constant rate. It is shown that the governing equations can be non-dimensionalized so that they do not involve any parameters and thus just one solution of the transformed boundary-layer equations is required. Series solutions which are valid both near the line source and far downstream are obtained and compared with the numerical solution of the full boundary-layer equations.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

Abbreviations

A :

constant, equation (29)

c :

specific heat

g :

acceleration due to gravity

k :

thermal conductivity

K :

permeability of the porous medium

L :

characteristic length

Pe :

Peclet number, equation (7)

q :

the constant rate of heat released from the line source,

Ra :

modified Rayleigh number for a porous medium, equation (7)

T :

temperature

u, v :

non-dimensional velocity components in thex- andy-directions

x, y :

non-dimensional coordinates

α :

thermal diffusivity

Β :

coefficient of thermal expansion

θ :

non-dimensional temperature

η,\(\hat \eta \),ξ,ζ :

similarity variables

Μ :

dynamic viscosity

v :

kinematic viscosity

ψ :

non-dimensional stream function

ξ :

a similarity variable

-:

dimensional variables,

′:

differentiation with respect toη,\(\hat \eta \) orζ

Ω :

centreline condition

∞:

ambient condition

References

  • Afzal, N., 1985, Two-dimensional buoyant plume in porous media: higher-order effects,Int. J. Heat Mass Transfer 28, 2029–2041.

    Google Scholar 

  • Cheng, P. and Zheng, T. M., 1986, Mixed convection in the thermal plume above a horizontal line source of heat in a porous medium of infinite extent, inHeat Transfer 1986, Hemisphere, Washington, DC, Vol. 5, 2671–2675.

    Google Scholar 

  • Hunt, R. and Wilks, G., 1981, Continuous transformation computation of boundary-layer equations between similarity regimes,J. Comp. Phys. 40, 478–490.

    Google Scholar 

  • Joshi, Y. and Gebhart, B., 1984, Vertical natural convection flows in porous media: calculations of improved accuracy,Int. J. Heat Mass Transfer 27, 69–75.

    Google Scholar 

  • Merkin, J. H., 1978, On solutions of the boundary-layer equations with algebraic decay,J. Fluid Mech. 88, 309–321.

    Google Scholar 

  • Nield, D. A. and White, S. P., 1992, Natural convection in an infinite porous medium produced by a line heat source, in A. McNabbet al. (eds),Mathematics and Models in Engineering Science, DSIR, Wellington, New Zealand, 121–128.

    Google Scholar 

  • Stewartson, K., 1957, On asymptotic expansions in the theory of boundary layers,J. Math. and Phys. 36, 173–191.

    Google Scholar 

  • Wooding, R. A., 1963, Convection in a saturated porous medium at large Rayleigh or Peclet number,J. Fluid Mech. 15, 527–544.

    Google Scholar 

  • Yih, C. S., 1965,Dynamics of Nonhomogeneous Fluid, Macmillan, New York.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pop, I., Ingham, D.B. & Miskin, I. Mixed convection in a porous medium produced by a line heat source. Transp Porous Med 18, 1–13 (1995). https://doi.org/10.1007/BF00620657

Download citation

  • Received:

  • Revised:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00620657

Key words

Navigation