Experimental data are presented from studies of turbulent heat transfer at high fluxes to water flowing in vertical tubes at supercritical pressures. A comparison of data for upward and downward flows indicates an effect of natural convection.
Get full access to this article
View all access options for this article.
References
1.
PowellW. B.‘Heat transfer in the region of critical temperature’, Jet Propul.195727 (No. 7), 776.
2.
BringerR. P.SmithJ. H.‘Heat transfer in the critical region’, A.I.Ch.E. Jl19573 (No. 1), 49.
3.
MiropolskiiZ. L.ShitsmanM. E.‘Heat transfer to water and steam with varying specific heat (in near critical regions)’, Zh. tekh. Fiz.1957XXVII (Issue 10), 2359.
ShitsmanM. E.‘Heat transfer to water, oxygen and CO2 in near critical region’, Teploenergetika19596 (No. 1), 68.
6.
HendricksR. C.GrahamR. W.HsuY. Y.MedeirosA. A.‘Correlation of hydrogen heat transfer in boiling and supercritical pressure states’, ARS Jl196232 (2), 277.
7.
ShitsmanM. E.‘Impairment of the heat transmission at supercritical pressures’, Teplofizika vysokikh temperature (High temperature)19631 (No. 2).
