A water insoluble material, when it is to be moved through a water phase to
be delivered into an oil phase, can be conveniently solubilized in a deter
gent micelle. In that form, it can exist in water at higher concentrations
and pass easily into the oil phase for which it has a higher affinity. We h
ave measured the mass transfer rates in water as well as those across the i
nterface. The mass transfer rates in such systems are very low which make t
hem difficult to measure. An experimental setup which is capable of making
these measurements is presented. A spatio-temporal variation of concentrati
on is induced inside a spectrophotometer cuvette. As the System moves towar
d equilibrium under diffusion, the change in concentration with time is mon
itored by measuring the absorbance of the solution. The solution to the app
ropriate boundary value problem is used to back calculate the diffusivity a
nd interfacial resistance from the absorbance data using the fact that abso
rbance is linearly dependent on concentration. Satisfactory values of diffu
sivities are reported for simple solutes and a surfactant, sodium dodecyl s
ulfate, SDS (the last has been reported earlier, Neogi, 1994) in water. Thi
s technique has been used to measure the transport of nitrobenzene from SDS
micelles to squalane. The results indicate significant interfacial resista
nce. A quantitative model has been provided for the first time.