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Characteristics of a double-diffusive interface at high density stability ratios

Published online by Cambridge University Press:  20 April 2006

T. A. Newell
T. A. Newell
Affiliation:
Department of Mechanical and Industrial Engineering, University of Illinois at Urbana-Champaign, 1206 West Green Street, Urbana. IL 61801
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Abstract

A thermohaline diffusive interface at large density stability ratios has been studied experimentally. Several interesting characteristics have been found. First, using a transient experiment technique, a transition from boundary-layer to core-regiondominated transport has been observed. Secondly, interface growth can occur through a series of steps owing to a sharp transition to a region with large interface growth rates. Thirdly, hysteresis occurs within the large density stability ratio region. Finally, the property-transport flux ratio increases as an interface switches from boundary- to core-dominated transports.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 149 , December 1984 , pp. 385 - 401
Copyright
© 1984 Cambridge University Press

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References

Crapper, P. F. 1975 Measurements across a diffusive interface. Deep-Sea Res. 22, 537–545.Google Scholar
Huppert, H. E. 1971 On the stability of a series of double-diffusive layers. Deep-Sea Res. 18, 1005–1021.Google Scholar
Huppert, H. E. & Linden, P. F. 1979 On heating a stable salinity gradient from below. J. Fluid Mech. 95, 431–464.Google Scholar
Lewis, W. T., Incropera, F. P. & Viskanta, R. 1982 Interferometric study of stable salinity gradients heated from below or cooled from above. J. Fluid Mech. 116, 411–430.Google Scholar
Lindberg, W. G. 1971 An upper bound on transport processes in turbulent thermohaline convection. J. Phys. Oceanogr. 1, 187–195.Google Scholar
Linden, P. F. & Shirtcliffe, T. G. L. 1978 The diffusive interface in double-diffusive convection. J. Fluid Mech. 87, 417–432.Google Scholar
Marmorino, G. O. 1974 Equilibrium heat and salt transport through a diffusive, thermohaline interface. M. S. thesis, Oregon State University.
Marmorino, G. O. & Caldwell, D. R. 1976 Heat and salt transport through a diffusive thermohaline interface. Deep-Sea Res. 23, 59–67.Google Scholar
Newell, T. A. & Boehm, R. F. 1982 Gradient zone constraints in a salt-stratified solar pond. Trans. ASMS: J. Solar Energy Engng 103, 280–285.Google Scholar
Poplawsky, C. J., Incropera, F. P. & Viskanta, R. 1981 Mixed layer development in a double-diffusive, thermohaline system. Trans. ASME: J. Solar Energy Engng 102, 351–359.Google Scholar
Saline Water Conversion Engineering Data Book 1971 M. W. Kellog Co., Piscataway, NJ.
Shirtcliffe, T. G. L. 1969 The development of layered thermosolutal convection. Intl J. Heat Mass Transfer 12, 215–222.Google Scholar
Shirtcliffe, T. G. L. 1973 Transport and profile measurements of the diffusive interface in double-diffusive convection with similar diffusivities. J. Fluid Mech. 57, 27–43.Google Scholar
Takao, S. & Narusawa, U. 1980 An experimental study of heat and mass transfer across a diffusive interface. Intl J. Heat Mass Transfer 23, 1283–1285.Google Scholar
Turner, J. S. 1965 The coupled turbulent transports of salt and heat across a sharp density interface. Intl J. Heat Mass Transfer 8, 759–767.Google Scholar
Turner, J. S. 1965 The behaviour of a stable salinity gradient heated from below. J. Fluid Mech. 33, 183–200.Google Scholar