MRS response with distributed array loops for 2D groundwater tomography

A new method for 2D groundwater tomography using Magnetic Resonance Sounding (MRS) with distributed array loops is described and the exciting field of the surface transmitter and the response from the spin magnetic field to the receivers are numerical calculated. To assess the effective effort in subsurface structure resolution by the use of 2D MRS surveys, a synthetic survey with distributed array receiver loop is modeled.