Abstract
The problem of double—diffusive convection for a thermohaline system consisting of a horizontal fluid layer situated above a saturated porous bed is studied experimentally. The porous bed is constructed from 5 mm spherical glass beads. The system initially contains a linear stabilizing salt distribution and is suddenly heated uniformly from below. The evolving temperature and concentration fields were determined at various times and were used to piece together a reliable picture of the behavior of the composite layer. The presence of the porous layer was responsible for a large delay in the flow initiation near the bottom wall, resulting in a considerable temperature increase. In some cases, the fluid saturating the porous matrix remained stagnant throughout the experiment and despite the fact that a vivid flow region existed directly above the porous region. The effect of the thermal Rayleigh number, the salinity Rayleigh number and the height of the porous substrate are also investigated in the course of the present study.
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Kazmierczak, M., Poulikakos, D. (1991). Transient Double Diffusive Convection in A Horizontal Fluid Layer Situated on Top of A Porous Substrate. In: Kakaç, S., Kilkiş, B., Kulacki, F.A., Arinç, F. (eds) Convective Heat and Mass Transfer in Porous Media. NATO ASI Series, vol 196. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-3220-6_21
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DOI: https://doi.org/10.1007/978-94-011-3220-6_21
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