Electromagnetic (EM) induction uses a transmitter to
generate a pulsed primary magnetic field. The transmitted magnetic field
induces eddy currents in nearby ferrous and non-ferrous metallic objects. The
EM measuring device senses the eddy current fields. The amplitude and phase of
the eddy current fields are related to the electrical properties of the
subsurface.
There are two types of Electromagnetic Induction
techniques commonly used. These are time-domain and frequency-domain.
Time Domain Electromagnetic Induction
The
time-domain instrument produces a short low energy electromagnetic pulse
from the transmitter coil. A receiver coil measures the decaying signal
induced into the ground with respect to time.
On completion of each
survey the dataset is downloaded to a computer for processing. The
data are used to produce site maps showing the locations and sizes of
detected anomalies.
The time domain method allows very sensitive detection of shallow and deep buried
metal objects It is capable of detecting and mapping the
location of both ferrous and non-ferrous buried metallic objects, large or
small. For example, it is capable of detecting a buried 55 gallon
drum at a depth of 3m.
Frequency Domain Electromagnetic Induction
The frequency domain instrument normally operates at a
fixed frequency. The generated signal creates small subsurface eddy
currents beneath the instrument. Automatic accurate measurements of the
components of the generated subsurface eddy currents are then used to
record changes in the subsurface soil conditions.
The frequency domain method is capable of
detecting and mapping any contaminant plume that is causing even a small
change in soil conductivity/resistivity. It can be used to find buried
dumpsites, leachate plumes, voids, underground streams and
aquifers and buried metallic/magnetic objects.