• Mapping and monitoring of saltwater / freshwater interface
• Groundwater investigations including aquifers
• Mineral-rich deposit exploration
• Deep geological mapping
• Design and feasibility of fluid infrastructure including levees and tailings dams
Transient Electro-magnetic (TEM) surveying uses the principle of electro-magnetic induction to measure changes in the electrical conductivity of the subsurface. An electric current of known frequency and magnitude is transmitted through a large coil which induces a magnetic field in the space surrounding the coil including the subsurface which in turn induces electrical currents (eddy currents) in the ground material. The transmitting current is then stopped and the rate of decay of the eddy currents is measured. The rate of decay is plotted as a curve and then inverted and analysed to determine the subsurface material conductivity with depth.
Electrical current is transmitted and recorded using coincident square loops. Loop size dictates vertical resolution and maximum depth of investigation with a larger loop providing deeper imaging with a lower vertical resolution. At each sounding location multiple readings are taken and stacked.
Data Analysis & Presentation
The acquired TEM data is displayed as a decay curve plotting the received voltage against time. The decay curves are inverted and constrained to obtain TEM soundings plotting conductivity with depth. Inversion of the TEM data can be constrained using the ERI data where both have been collected. Other sources for constraining the inversion may include downhole conductivity logs and groundwater monitoring wells which can be used if available.
Where multiple adjacent TEM sounds have been made, continuous profiles can be generated showing the variation with conductivity with depth and laterally along the profile.