the underground geological environment and structure are becoming more complex
and the difficulty of detection increases sharply. Therefore
the multi-channel transient electromagnetic method is introduced to study the three-dimensional model
thereby laying a good foundation for actual resource exploration. Aiming at the exploration characteristics of the multi-channel transient electromagnetic method
firstly
the working principle and outstanding characteristics of the multi-channel transient electromagnetic method are introduced
and the second is the research and analysis of its forward and inverse theory. Research shows that the frequency domain response of the transient electromagnetic field can be obtained through the time-frequency conversion method
and then the time domain response can be inverted by the conjugate gradient method. Finally
a three-dimensional model combining high resistance and low resistance is used for inversion simulation
and draw isochronous curves. Analyzing the inversion results
it can be seen that the multi-channel transient electromagnetic method has good response to the three-dimensional model and the boundary description. It can truly reflect the shape of the anomaly
which proves that the multi-channel transient electromagnetic method can be a reflection of the anomaly effective means.