ELECTROPHORETIC MOBILITY OF A SEMIDILUTE SUSPENSION OF SPHERICAL-PARTICLES WITH THICK DOUBLE-LAYERS AND LOW ZETA-POTENTIAL

Authors
Citation
J. Ennis et Lr. White, ELECTROPHORETIC MOBILITY OF A SEMIDILUTE SUSPENSION OF SPHERICAL-PARTICLES WITH THICK DOUBLE-LAYERS AND LOW ZETA-POTENTIAL, Journal of colloid and interface science, 185(1), 1997, pp. 157-173
Citations number
45
Categorie Soggetti
Chemistry Physical
ISSN journal
00219797
Volume
185
Issue
1
Year of publication
1997
Pages
157 - 173
Database
ISI
SICI code
0021-9797(1997)185:1<157:EMOASS>2.0.ZU;2-O
Abstract
The electrophoretic mobilities of two spherical particles are analysed for the case where the electrical double layer is no longer thin with respect to the particle sizes, but the zeta potentials on the particl es are low. Using a method of reflections, we obtain the mobilities as a power series in 1/r(12) up to O(r(12)(-10)) (where r(12) is the cen ter-to-center separation of the spheres), with the proviso that the do uble layers on the two particles do not overlap. Unlike the case of th in double layers, there is now a nonzero interaction between identical particles. The first term in the interaction is O(r(12)(-3)), but the coefficient becomes large for thick double layers. An expression for the average mobility of a mildly polydisperse suspension of spheres wi th thick double layers is then derived correct to first order in the v olume fraction of the spheres. The results of the reflection calculati on are then used to obtain an approximate evaluation of this expressio n. It is found that the first order effect for thick double layers is significantly larger than it is for thin double layers, and that the a verage effect of polydispersity in size or surface potential is weak u nless the double layers are quite thick. For a monodisperse suspension , an expression is obtained for the mean square deviation of the parti cle velocity from the mean velocity. An approximate evaluation of this expression using the reflection results shows that the magnitude of t he mean square fluctuations in the direction of the applied field can be significantly larger than that in the transverse direction. (C) 199 7 Academic Press