The effect of vertical throughflow on the onset of convection, induced by an applied vertical temperature gradient in a vertical cylinder is studied analytically using linear stability theory. This problem is important to hydrologists to investigate under what conditions convection is taking place in a well or borehole. The effect of double diffusion is included. Both nonoscillatory and oscillatory situations are studied.
The Onset of Double-Diffusive Convection in a Vertical Cylinder With Vertical Throughflow
Contributed by the Heat Transfer Division of ASME for publication in the Journal of Heat Transfer. Manuscript received March 16, 2012; final manuscript received September 5, 2012; published online February 8, 2013. Assoc. Editor: Jose L. Lage.
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Nield, D. A., and Kuznetsov, A. V. (February 8, 2013). "The Onset of Double-Diffusive Convection in a Vertical Cylinder With Vertical Throughflow." ASME. J. Heat Transfer. March 2013; 135(3): 034502. https://doi.org/10.1115/1.4007859
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