
The Frequency Domain Electromagnetic (FDEM) method is a noninvasive geophysical technique for analyzing the electrical and magnetic properties of the subsurface through electromagnetic induction.
The system consists of two coils: a transmitter (Tx), which generates an alternating electromagnetic field of known frequency, and a receiver (Rx), which measures the ground response. When the primary field passes through the ground, it induces electric currents in the conductive materials. These currents, in turn, generate a secondary field, the intensity of which depends on the electrical conductivity of the medium.
The method allows two components to be measured:
- The quadrature component, used to calculate the apparent electrical conductivity;
- The in-phase component, which is sensitive to magnetic susceptibility and the presence of metallic materials.
FDEM is a rapid technique suitable for detailed mapping of large portions of land.
Fields of Application:
Archaeological research
Contaminant mapping
Hydrogeological research
Metal object search
Fields of Application:
Archaeological research
Contaminant mapping
Hydrogeological research
Metal object search
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