Results from a grid-mixing experiment in a diffusive thermohaline syst
em are described. A model is proposed to separate the effects of inter
facial flux and interfacial movement (entrainment) on property changes
in the mixed layer and the present results for heat and salt fluxes a
re compared with previous studies in unstirred diffusive systems. Comp
arison of an eddy time-scale and a time-scale for development of insta
bility in the interfacial boundary layers suggests a means of determin
ing whether stirring or double-diffusive instability controls the inte
rfacial transports. For the present conditions there was a negligible
effect of diffusive stratification on entrainment rates, and interfaci
al fluxes were increased by the stirring. It is suggested that the rat
io R(F)/R(rho), where R(F) is the interfacial flux ratio and R(rho) is
the interfacial stability ratio, should be a function of the overall
bulk Richardson number, Ri.