Molecular dynamics simulations of the interior of aqueous reverse micelles

Citation
J. Faeder et Bm. Ladanyi, Molecular dynamics simulations of the interior of aqueous reverse micelles, J PHYS CH B, 104(5), 2000, pp. 1033-1046
Citations number
98
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF PHYSICAL CHEMISTRY B
ISSN journal
15206106 → ACNP
Volume
104
Issue
5
Year of publication
2000
Pages
1033 - 1046
Database
ISI
SICI code
1520-6106(20000210)104:5<1033:MDSOTI>2.0.ZU;2-K
Abstract
Aqueous reverse micelles, which are surfactant aggregates in nonpolar solve nts that enclose packets of aqueous solution, have been widely studied expe rimentally and theoretically, but much remains unknown about the properties of water in the interior. The few previous molecular dynamics simulations of reverse micelles have not examined how the micelle size affects these pr operties. We have modeled the interior of an aqueous reverse micelle as a r igid spherical cavity, treating only the surfactant headgroups and water at a molecular level. Interactions between the interior molecules and the cav ity are represented by a simple continuum potential. The basic parameters o f the model-micelle size, surface ion density, and water content-are based on experimental measurements of Aerosol OT reverse micelles but could be ch osen to match other surfactant systems as well. The surfactant head is mode led as a pair of atomic ions a large headgroup ion fixed at the cavity surf ace and a mobile counterion. The SPC/E model is used for water. The simulat ions indicate that water near the cavity interface is immobilized by the hi gh ion concentration. Three structural regions of water can be identified: water trapped in the ionic layer, water bound to the ionic layer, and water in the bulklike core. The basic properties of bulk water reemerge within a few molecular layers. Both the structure and dynamics of water near the in terface vary with micelle size because of the changing surface ion density. The mobility of water in the interfacial layers is greatly restricted for both translational and rotational motions, in agreement with a wide range o f experiments.