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Transient electrophoresis of a charged porous particle
Author(s) -
Lai Yi C.,
Keh Huan J.
Publication year - 2020
Publication title -
electrophoresis
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.666
H-Index - 158
eISSN - 1522-2683
pISSN - 0173-0835
DOI - 10.1002/elps.201900413
Subject(s) - electrophoresis , debye length , dimensionless quantity , particle (ecology) , permeability (electromagnetism) , materials science , electric field , chemistry , mechanics , physics , chromatography , ion , membrane , oceanography , biochemistry , organic chemistry , geology , quantum mechanics
The starting electrophoretic motion of a porous, uniformly charged, spherical particle, which models a solvent‐permeable and ion‐penetrable polyelectrolyte coil or floc of nanoparticles, in an arbitrary electrolyte solution due to the sudden application of an electric field is studied for the first time. The unsteady Stokes/Brinkman equations with the electric force term governing the fluid velocity fields are solved by means of the Laplace transform. An analytical formula for the electrophoretic mobility of the porous sphere is obtained as a function of the dimensionless parameters κ a , λ a ,ρ p / ρ , and ν t / a 2 , where a is the radius of the particle, κ is the Debye screening parameter, λ is the reciprocal of the square root of the fluid permeability in the particle, ρ p and ρ are the mass densities of the particle and fluid, respectively, ν is the kinematic viscosity of the fluid, and t is the time. The electrophoretic mobility normalized by its steady‐state value increases monotonically with increases in ν t / a 2and κ a , but decreases monotonically with an increase inρ p / ρ , keeping the other parameters unchanged. In general, a porous particle with a high fluid permeability trails behind an identical porous particle with a lower permeability and a corresponding hard particle in the growth of the normalized electrophoretic mobility The normalized electrophoretic acceleration of the porous sphere decreases monotonically with an increase in the time and increases with an increase in λ a from zero at λ a = 0 .