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Nonlinear Analysis of Cross Rolls of Electrically Conducting Fluid under an Applied Magnetic Field with Rotation

  • Y. Rameshwar
  • , G. Srinivas
  • , A. Krishna Rao
  • , U. S. Mahabaleshwar
  • , D. Laroze
  • Osmania University
  • Universidad de Tarapacá
  • Davangere University

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

Abstract

The proposed planer layer dynamo physical model has real-world applications, especially in the Earth’s liquid core. Thus, in this paper, an attempt is made to understand the finite amplitude convection when there exists a coupling between the Lorentz force and the Coriolis force. In particular, the effect of a horizontally applied magnetic field is studied on the Rayleigh–Bénard convection (RBC) that contains the electrically conducting fluid and rotates about its vertical axis. Free–free boundary conditions are assumed on the geometry. Attention is focused on the nonlinear convective flow behavior during the occurrence of cross rolls which are perpendicular to the applied magnetic field and parallel to the rotation axis. The visualization of cross rolls is achieved using the Fourier analysis of perturbations up to the O((Formula presented.)). The relationship of the Nusselt number ((Formula presented.)) with respect to the Rayleigh number (R), the Ekman number (E), and the Elsasser number ((Formula presented.)) is investigated. It is observed that E generates a strong damping effect on the flow velocity and on the heat transfer at high rotation rates. Using the heatline concept, it is observed that the temperature within the central regime is enhanced as the (Formula presented.) increases. The results show that either E decreases or (Formula presented.) increases, then the heat transfer rate increases.

Original languageEnglish
Article number1945
JournalProcesses
Volume11
Issue number7
DOIs
StatePublished - Jul 2023

Keywords

  • cross rolls
  • earth’s liquid core
  • electrically conducting fluid
  • nonlinear convection
  • planar layer dynamos

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