Abstract

The effect of thermal parameters on the flow temperature of a magnetized plasma in a sphere was studied. The study models astrophysical environments such as the Sun, which have spherical outline. The governing equations of the problem were obtained based on the Navier-Stokes equations under the Boussinesq’s approximation. The solutions to the resulting equations were sought by means of the general perturbation method and the results were graphically represented with radial distance, r = 1.0 on the figures corresponding to the surface of the sphere. The thermal parameters; particularly, the radiation parameter, N2 and free convection parameter, Gr. were investigated in this study with a view to determine the effect of varying these parameters on the plasma flow temperature. Increasing both N2 and Gr. led to a decrease in the plasma flow temperature in the sphere. However, above the sphere (i.e. at radial distances, r >1.0) where the plasma density is sparse, increasing N2 and Gr. produced a corresponding increase in the plasma flow temperature. The decrease in the plasma flow temperature within the sphere with increase in the thermal parameters was observed to be more significant between radial distances, r = 0.25 and r = 0.7 (i.e., 0.25 ≤ r ≤ 0.7) than between r = 0.7 and r = 1.0 (i.e., 0.7 ≤ r ≤ 1.0). This is attributable to the prevalence of partially ionized heavy elements within 0.7 ≤ r ≤ 1.0 (corresponding to the convection zone of the solar interior) which trap the high energy photons thereby reducing the rate of radiative heat loss.

Highlights

  • The Sun ispowered with the ability to replenish the huge amount of energy lost to solar space from the nuclear fusion process at the core

  • The thermal parameters of interest investigated in this study were seen to significantly influence the temperature distribution in the solar sphere

  • Above the sphere where the plasma density is sparse, increasingthe radiation and free convection parameters produced a corresponding increase in the plasma flow temperature

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Summary

Introduction

The Sun ispowered with the ability to replenish the huge amount of energy lost to solar space from the nuclear fusion process at the core. Of the very high temperature of about 1.5 x 107 K at the core of the Sun, the temperature at the solar surface is only about 5,780 K. It means that most of the energy is lost on the way to the solar surface. The high temperature differential between the core and surface of such bodies induce radiative and convective heat transfer. Energy transmission through the plasma of the solar interior is mainly by means of radiation and convection [4]. This suggests that the dynamics of radiation and convection allow for the progressive reduction in the transmitted energy

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