FORCED-CONVECTION HEAT AND MASS TRANSFER FROM COMPLEX SURFACES
- 1 July 1990
- journal article
- research article
- Published by Taylor & Francis in Experimental Heat Transfer
- Vol. 3 (2) , 83-100
- https://doi.org/10.1080/08916159008946379
Abstract
Heat and mass transfer rates from complex surfaces to a turbulent channel flow were measured using an infrared imaging system and the naphthalene sublimation technique, respectively. The surfaces are composed of spherical particles embedded either in a layer of thermally conducting, nonevaporating liquid or in an isothermal layer of subliming naphthalene. The experimental results indicate that, in general, the surface heat and mass transfer coefficients vary as the surface roughness increases, whereas the surface heat transfer coefficient changes as the solid-to-liquid thermal conductivity ratio is varied. Mass transfer rates exhibit less sensitivity to variations in the naphthalene height for surfaces composed of smaller particles, and heat transfer rates from surfaces of smaller particles remain fairly constant as the liquid level and thermal conductivity ratios are varied. The results are discussed relative to drying of partially wetted surfaces with surface complexity induced by the presence of droplets upon an impermeable substrate or a receding moisture front in a bed of granular material.Keywords
This publication has 6 references indexed in Scilit:
- FORCED CONVECTION HEAT AND MASS TRANSFER FROM A PARTIALLY LIQUID-COVERED SURFACENumerical Heat Transfer, Part A: Applications, 1989
- On the mechanism of the constant drying rate period and its relevance to diffusion controlled catalytic gas phase reactionsChemical Engineering Science, 1988
- Turbulent duct flow with streamwise nonuniform heating at the duct wallInternational Journal of Heat and Mass Transfer, 1987
- Heat and mass transfer in wood during dryingInternational Journal of Heat and Mass Transfer, 1985
- ON THE MECHANISM OF DRYING OF GRANULAR BEDSJOURNAL OF CHEMICAL ENGINEERING OF JAPAN, 1968
- Sublimation From Disks to Air Streams Flowing Normal to Their SurfacesTransactions of the American Society of Mechanical Engineers, 1958