The signal measured in a Magnetic Resonance Sounding (MRS) is of very low amplitude, of the order of tens of nanovolts and is very easily disturbed by the presence of electromagnetic noise of industrial or natural origin. To expand the capabilities of this new geophysical method, it is of great importance to develop field and analytical techniques to reduce the influence of noise in the final results of the MRS. Some field techniques are analyzed in this paper, for several MRS taken in a noisy area at a detrital aquifer in the south of Spain. Two kinds of noise are present, both of amplitude higher than 1500 nV: continuous random noise and spiky noise, with bursts of very high amplitude and occurrence depending on the site and on the time of the day. Trial records made at these places are of little significance, and only complete records taken with the most suitable size, shape and orientation of the antenna, and with a large stacking number, allow to detect the decay pattern of the signal coming from the water-rich layers. The appropriate design of these recording parameters have proven capable of diminishing the effect of random noise, but the results are not as good for spikes, which demand the use of different techniques. The knowledge of the noise pattern obtained in the MRS measurement could be used to design digital filters to attenuate noise influence, together with the aid of surgical muting. The interpretation of the field data has been made without any prior knowledge of the geological information. Despite the high noise level observed on this site, the inversion result achieved present a remarkable correlation with geological data for the water content distribution and are worse for the decay time determination, which seems to be more affected by the existence of noise. Phase and frequency seem to be good quality control parameters before inverting the data, regardless the noisy aspect of the recorded values.
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