
Tuesday, 7 October 2008: 10:45 AM
George R. Brown Convention Center, 362F
Electrical impedance spectroscopy was used to study the behavior of water in sandy soils.
In these studies, impedance and its phase angle were measured between 100 Hz and 100 MHz.
The data were transformed into Cole-Cole plots which reveal several relaxation mechanisms
over this frequency range. In addition, loss tangent graphs indicate that there is more
dispersion with frequency in moist sand samples than in free water indicating that the water
is bound differently in the sand than in bulk water. Finally, the graph of relaxation time
versus dielectric constant indicates how tightly the water is being held for each mechanism.