The Earth's pulse and the Schumann frequency

by Paulo N. Correa, Alexandra N. Correa
Aurora Biophysics Research Institute

J Aetherom Res, Volume 4, Issue 15 (August 2026),  pp. 1-17

Article ID:   JAR04-15-01

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ABSTRACT The Correas provide experimental evidence that the Schumann frequency is not a characteristic of the ionospheric cavity per se, nor an electromagnetic function. Instead, using a three-band analyzer spanning 1 to 13 cps, they show that it can be picked up by an isolated ground connection inside a Faraday Cage room, and that, accordingly, it is a geo- acoustic electric signature. The authors present a novel hypothesis on its causation that accounts for its presence in the crust, oceans and atmosphere. They suggest that the main Schumann frequency strikes a C0 tone at 8.0054 cps, rather than at 7.83 cps, and that the intercalation frequency of the damped wave responsible for the spectrum of the six Schumann resonances is A0 = 6.6711 cps. In line with the authors' published model of a 1,512 eV terrestrial geoplasma originating at the Earth's core, they propose that the last (or 6th) Schumann resonance strikes at 41.36 cps = E1, corresponding to the acoustic signature of the terrestrial ambipolar radiation that drives the geoplasma.