2006, Vol.9, No.3, pp.265-268
The measured conductivity of the clay-water samples at different water contents show
scaling behavior in the low frequency limit with the power-law frequency dependence.
The attempt to explain the experimentally observed features is presented considering
the stochastic motion of the ion near the particle-fluid interface described by the fractional
Langevin equation.
Key words:
dielectric spectroscopy, porous media, conductivity, fractional dynamics
Full text: Acrobat PDF (157KB)
Copyright © Nonlinear Phenomena in Complex Systems. Last updated: September 6, 2006