Surface tension of an anionic surfactant: Equilibrium, dynamics, and analysis for Aerosol-OT

Citation
Ss. Datwani et Kj. Stebe, Surface tension of an anionic surfactant: Equilibrium, dynamics, and analysis for Aerosol-OT, LANGMUIR, 17(14), 2001, pp. 4287-4296
Citations number
16
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
LANGMUIR
ISSN journal
07437463 → ACNP
Volume
17
Issue
14
Year of publication
2001
Pages
4287 - 4296
Database
ISI
SICI code
0743-7463(20010710)17:14<4287:STOAAS>2.0.ZU;2-W
Abstract
The equilibrium and dynamic surface tension of sodium bis(2-ethylhexyl) sul fosuccinate (Aerosol-OT) are studied as a function of concentration and ion ic strength controlled by the addition of either the monovalent salt sodium chloride or the divalent salt calcium chloride. These data are compared to a surfactant mass-transfer model with a quasi-equilibrium treatment of the electrostatics. The Davies adsorption isotherm and surface equation of sta te relate the bulk concentration, surface concentration, and surface tensio n. At equilibrium, the surface concentration increases with the ionic stren gth of the electrolyte, so the surface tension reduces more strongly. The d ata at all ionic strengths are well described by the Davies model. Because the characteristic diffusion time scale increases as the square of the surf ace concentration, an increasing equilibration time with ionic strength mig ht be anticipated for this molecule. However, the time required for the sur face tension relaxation observed in experiment is fairly insensitive to cha nges in the ionic strength over the range of surfactant concentrations stud ied for both monovalent and divalent electrolytes at fixed surfactant bulk concentration. When these data are compared to a full integration of the su rfactant transport equations, they are found to agree with a diffusion-cont rolled mass-transfer mechanism. The key issue behind the apparently contrad ictory behavior of increased adsorption resulting in lower equilibrium surf ace tensions, while diffusion time scales remain essentially unchanged, is the high surface activity of Aerosol-OT. Even at the most dilute concentrat ions studied, Aerosol-OT adsorbs close to its maximum packing limit. The su rface concentration increases weakly near this value with ionic strength. T herefore, the diffusion time scale also changes weakly. Concomitantly, the equilibrium surface tension changes strongly because it is highly sensitive to small changes in surface concentration near this limit.