HAIT Journal of Science and Engineering B, Volume 2, Issues 1-2, pp. 125-167 Copyright C 2005 Holon Academic Institute of Technology ° Primordial hydrogen-helium degassing, an overlooked major energy source for internal terrestrial processes 1, 2 Arie Gilat ∗ and Alexander Vol 1Geological Survey of Israel (ret.), 8 Yehoash St., Jerusalem 93152, Israel 2Enlightment Ltd. 33 David Pinsky St., Haifa 34454, Israel ∗Corresponding author:
[email protected] Received 20 July 2004, revised 3 February 2005, accepted 16 February 2005 Abstract The currently accepted theories concerning terrestrial processes are lacking in accounting for a source of internal energy which: (a) are quickly focused, e.g. earthquakes and volcanic eruptions; (b) are of very high density; (c) provide very high velocities of energy re- lease; (d) have very high density of the energy transport and relatively small losses during transportation over long distances; (e) are quasi- constantly released and practically limitless. This energy release is always accompanied by H- and He-degassing. Solid solutions of H and He, and compounds of He with H, O, Si and metals were discovered in laboratory experiments of ultra-high PT-conditions; He-S, He-Cl, He- C, He-N structures can be deduced from their atomic structure and compositions of natural He-reach gases. Ultra-high PT-conditions ex- ist in the Earth’s interior; hence it seems most likely that some “exotic” compounds are present in the Earth’s core and mantle. During Earth’s accretion, primordial hydrogen and helium were trapped and stored in the planet interior as H- and He- solutions and compounds, stable only under ultrahigh PT-conditions that were dis- covered in recent experiments.