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In this article a way is indicated for the determination of the soils constants, based upon measurements of both the electric and the magnetic field (remote from but also in the vicinity of the emitter). The method is based especially upon the different behaviour of the electric and magnetic field as a function of the distance in the vicinity of the emitter. Owing to this difference and its mathematical form it will be possible to derive the required constants of the earth by means of one simple system of curves, which may be used again in every other case, as the curves do not depend upon the distances of the points of observation from the emitter. This greatly simplifies the solution of the problem.

The earth's constants from combined electric and magnetic measurements partly in the vicinity of the emitter