Authors: Frank H. Makinson
Electromagnetic geophysical studies have been using very low electromagnetic frequencies, below 1 Hz, transmitters and receivers for several decades. The devices that produce these frequencies are referred to as magnetotelluric transmitters and receivers. The frequencies for these devices are being identified by using a decimal notation, 0.1, 0.01, 0.001, 0.0001, 0.00001 Hz and below. Accepting frequency designations as tens divisions of one reveals that the current EM frequency scale is nonlinear. There is not a mathematically equivalent relationship if they both are not expressed in unit values. Because of this lack of equivalency, all contemporary physical law equations that contain frequency directly or indirectly are invalid.
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