The present paper mathematically establishes that rotatory thermohaline convection of the Veronis type in porous medium cannot manifest itself as oscillatory motion of growing amplitude in an initially bottom heavy configuration if the thermohaline Rayleigh number Rs, the Lewis number t, the Prandtl number p1, the porosity ?, satisfy the inequality Rs = 4p2 (1/Pl + t/(E'?p1 )) , where Pl and E' are constants which depend upon porosity of the medium. It further establishes that this result is uniformly valid for the quite general nature of the bounding surfaces.
Cite this article:
Jyoti Prakash, Sanjay Kumar Gupta. A Characterization Theorem in Rotatory Thermohaline Convection of Veronis Type in Porous Medium. Research J. Engineering and Tech. 3(2): April-June 2012 page133-139.