This work is focused on steady, laminar, coupled heat and mass transfer by natural convect ive boundary layer ow over a permeable isothermal truncated cone in the presence of magnetic eld and radiation effect s. A suitable set of dimensionless variables is used and nonsimilar equations governing the problem are obtained. The resulting equations have the property that they reduce to various special cases previously considered in the literature. An adequate implicit, tridiagonal nite difference scheme is employed for the numerical solution of the obtained equations. Various comparisons with previously published work are performed and the results are found to be in excellent agreement. Represent ative results for the velocity, temperature, and concentration pro les as well as the local skin-friction coef cient; local Nusselt number and the local Sherwood number illustrating the in uence of the Hartmann number; the concentration to thermal buoyancy ratio; and the wall mass transfer coef cient are presented and discussed.
INTROD UCTIONThis article deals with steady, laminar, heat and mass transfer by natural convection hydromagnetic boundary layer £ow around an isothermal permeable truncated cone. This £ow and heat transfer situation is of considerable interest because it can occur in many geothermal, geophysical, technological, and engineering applications such as nuclear reactors, migration of moisture through air contained in ¢brous insulations, grain storage, nuclear waste disposal, dispersion of chemical pollutants through water-saturated soil, and others. The geothermal gases are electrically conducting and are affected by the presence of a magnetic ¢eld. The same is found regarding the cooling of nuclear reactors (see Aldoss et al. [1]).The natural convection heat transfer mode in various geometries has received a great deal of attention. For example, Kao [2] has reported on the local nonsimilarity solution for laminar natural convection adjacent to a vertical surface. Na [3] has considered natural convective £ow past a nonisothermal vertical £at plate and reported a numerical solution. Lin and Chen [4] have studied mixed convection on a vertical plate for £uids on any Prandtl number. The laminar natural convection