Non-contact measurement of ground conductivity is a standard method in
geophysics and archaeology. What is usually used is the "Slingram method". In
that method, an AC signal is sent to a small coil, and the induced voltage is
measured in a second sensing coil a short distance away. The effective depth of
the measurement can be controlled by how far apart the coils are (typical
distance between coils is 1-2 meters). In a typical measurement, the coils are
placed on or just above the ground, and the device is moved to measure
conductivity along a line or grid. A contour map of conductivity can then be
generated to locate buried features. A long time ago I played around with one
of these devices (my father is in archaeology).
The problem with adapting this for use with antennas is that the analysis is
done assuming the DC limit. Typical measurements are done at something like 10
KHz. A quick google search did find some work at getting this to work in the
few-MHz region, but the analysis there is not simple.
Tor N4OGW
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