Free Convection Effects on the Hydromagnetic Oscillatory Flow in the Stokes Problem Past an Infinite Porous Vertical Limiting Surface with Constant Suction - Part Two

Details Free Convection Effects on the Hydromagnetic Oscillatory Flow in the Stokes Problem Past an Infinite Porous Vertical Limiting Surface with Constant Suction - Part Two Free Convection Effects on the Hydromagnetic Oscillatory Flow in the Stokes Problem Past an Infinite Porous Vertical Limiting Surface with Constant Suction - Part Two

Aug 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981ap%26ss..78..157k&link_type=abstract

Astrophysics and Space Science, Volume 78, Issue 1, pp.157-168

Astronomy and Astrophysics

Astrophysics

Scientific paper

Unsteady hydromagnetic boundary layer flow of a viscous incompressible and electrically conducting fluid past an infinite vertical non-conducting porous limiting surface in presence of a transverse magnetic field, is considered when the limiting surface is moving impulsively in its own plane and is subjected to a constant suction. The free stream oscillates in time about a constant mean value and the magnetic Reynolds number is taken to be small enough so that the induced magnetic field is negligible. As the mean steady flow has been presented in Part I, only the solutions for the transient velocity profiles, transient temperature profiles, the amplitude and the phase of the skin friction and the rate of the heat transfer are presented in this work. The influence of the various parameters entering into the problem, especially of the magnetic parameterM, is extensively discussed. A comparative study with hydrodynamic case (M=0) is also made.

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