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Effect of horizontal thermal gradient on double-diffusive ferroconvection

IR@NISCAIR: CSIR-NISCAIR, New Delhi - ONLINE PERIODICALS REPOSITORY (NOPR)

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Field Value
 
Creator Sekar, R
Vaidyanathan, G
Hemalatha, R
 
Date 2009-03-23T07:18:00Z
2009-03-23T07:18:00Z
2009
 
Identifier 0019-5596
http://hdl.handle.net/123456789/3441
 
Description 192-198
The effect of horizontal thermal and salinity gradients on ferroconvection of a double diffusive system subjected to two dimensional magnetic fields with compensating horizontal thermal and solutal gradients has been investigated. Assuming that the fluid layer is bounded by free boundaries, the conditions for the onset of stationary and oscillatory instabilities are established using linear theory and normal mode technique. Wide range of values of the ratios of horizontal and vertical gradients with respect to temperature, salinity and the cell size are considered. It has been found that the system stabilizes only through oscillatory mode for ratios of the temperature and salinity gradients which tend to make the cell size greater than 1. Stationary instability is found to occur for the ratios of the temperature and salinity gradients which tend to make the cell shape smaller than 1.
 
Language en_US
 
Publisher CSIR
 
Source IJPAP Vol.47(03) [March 2009]
 
Subject Double diffusive
Magnetic field
Horizontal temperature
Salinity gradients
Linear stability
Cell size
 
Title Effect of horizontal thermal gradient on double-diffusive ferroconvection
 
Type Article