A known uniform magnetic field can be created in the center of a solenoid. We constructed a solenoid three meters long, with a radius of 0.65 m, which was big enough for the TEM field coils to fit inside. Data procedures were tested in a miniature version in which scale-model coils, used for physical scale modeling in the University of Southern Maine geophysical laboratory, were calibrated in a small solenoid. An HP35665 Dynamic Signal Analyzer was used to transmit a sweep of frequencies from 10 Hz to 51.4 kHz through the windings of the solenoid. This instrument then collected voltages across a known resistor, providing the transmitted current, and voltages from the TEM receiver coil inside the solenoid, yielding the coil's response. Corrections were then made numerically to field TEM data collected in Gray.
The Gray delta is a glaciofluvial outwash delta, comprised of fine- to medium-grained unconsolidated sands. Bedrock beneath the delta is a granite of the Sebago Lake pluton. TEM results showed that the delta has a resistivity of about 400 ohm-m and is approximately 30 m thick correlating well with seismic refraction data and information from nearby wells.