Dewatering of super-soft kaolin clay (Lamont-Black, 2001; Jones
et al., 2002).
Water flows by electroosmosis from the anode to the cathode thus the area
around the anode experiences the greatest reduction in moisture content and
improvement in shear strength. In order to minimise moisture content anisotropy,
the trial was completed with a phase of polarity reversal in order to draw
water away from the electrodes which were acting as anodes in the first phase.
Polarity reversal resulted in a much more even distribution of shear strength
in the test soil.

Consolidation - normal and reverse polarity (1.5m depth)
- The bottom axis above represents distance along the length of the test pit
- The grey background of the graph represents a cross section of the soil
- The blue vertical lines represent cathodes and the red line represents the anodes at the start i.e. during normal polarity. These swapped over during reverse polarity
- Plots of undrained shear strength, on different dates, measured at 1.5m depth along the long axis of the test pit
At the end of the normal polarity phase, a distinct difference was seen in the strengths between the anode and cathode areas. Polarity reversal was used to ‘smooth out’ these differences. This resulted in a flatter curve. Part of this process also improved the shear strength of the soil immediately ‘beyond’ the treatment ( i.e. in the non electroosmotic zone ) from approximately 6kPa to between 10 and 15kPa.
This test shows the potential for the use of EKG for ground improvement by consolidating materials such as alluvial clays and silts in low lying or flood plain areas.
