A transport theory and supporting experiments are detailed for the adsorption of surfactant from micelle solutions onto a clean air/water interface. The study focuses on adsorption from very dilute solutions consisting of globular aggregates. In the usual mechanism conceived for the adsorption process, when a clean interface is created in the solution of monomer and globular aggregates, monomer initially kinetically adsorbs from the sublayer onto the surface, depleting the sublayer concentration of monomer. This depletion, as it perturbs the micelle/monomer equilibrium, is followed by the disassembly of aggregates in the sublayer (to replenish monomer). Co-currently, aggregates and monomer diffuse from the bulk to the depleted sublayer. Thus in this classical picture, while the micelles provide a reservoir for monomer adsorption by their disassembly – and thereby enhance the adsorption rate – they provide no direct route for adsorption. Using this picture as a starting point, in this study an asymptotic transport theory is constructed for the case in which the time scale for the diffusion of the monomer is much slower than the time scale for the kinetic breakdown of the aggregates. With this separation of time scales, disassembly of micelles takes place only along a boundary separating regions without micelles (micelle-free zones) from regions containing micelles. In the regions containing micelles, the larger rate of disassembly relative to the rate of diffusion of monomer maintains the monomer concentration at the critical aggregate concentration ( C CAC). Two regimes arise: in the first, at low aggregate concentrations, micelle diffusion cannot keep up with the kinetic surface adsorption of monomer, and a micelle-free zone emerges from the surface and moves into the bulk. Micelles diffuse from the bulk to the boundary of the zone, break-up and monomer diffuses through the micelle-free zone and kinetically adsorbs onto the surface. In the second regime, at higher aggregate concentrations, the micelle diffusive flux is commensurate with the kinetic rate of monomer surface adsorption, and a micelle-free zone does not form. Micelles diffuse directly to the surface, and break-up in the sublayer; monomer then kinetically adsorbs onto the surface. The adsorption rate is limited only by the kinetics of monomer adsorption since the monomer sublayer concentration is equal to the C CAC, and represents the fastest rate that surfactant can adsorb onto the surface in the absence of diffusion barriers. Numerical solutions are obtained for a polyethoxylated surfactant C 14E 6 whose micelle disassembly time scale satisfies the requirement that it be faster than the diffusion time scale of the monomer. For C 14E 6 the monomer adsorption parameters and diffusion coefficient of monomer are obtained from separate dynamic tension measurements below the C CAC; the micelle diffusion coefficient is estimated from the literature. A critical total surfactant concentration of 4.25 C CAC is computed, below which a micelle-free zone forms and above which the zone does not form, and surface concentrations and tension reductions as a function of time are simulated for both regimes. Experiments are undertaken in which dynamic tensions are measured for adsorption of surfactant onto an initially clean interface from C 14E 6 micelle solutions using the pendant bubble method. These experiments show that below the critical value of 4.25 C CAC, the theory predicts the experimental tension relaxations in excellent agreement and no adjustable constants. Above the critical value, relaxations continue to accelerate with bulk concentration, and become faster than the kinetically-dictated fastest relaxation. This implies an alternate route to surfactant adsorption; since micelles are present in the sublayer in the second regime (and are not in the first regime), we suggest that they directly supply monomer to the surface.
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