Background for Terrestrial Antineutrino Investigations: Radionuclide Distribution, Georeactor Fission Events, and Boundary Conditions on Fission Power Production
J. Marvin Herndon, Dennis A. Edgerley

TL;DR
This paper estimates Earth's internal radionuclide distribution, explores the potential for natural nuclear fission reactors at the core, and models georeactor power limits and fuel composition.
Contribution
It provides new estimates of radionuclide locations within Earth and numerical simulations of georeactor power and composition, advancing understanding of Earth's internal nuclear processes.
Findings
Most K-40 may be in the lower mantle silicates.
Earth's core could host self-sustaining nuclear fission.
Maximum georeactor power is 30 terawatts.
Abstract
Estimated masses of fissioning and non-fissioning radioactive elements and their respective distributions within the Earth are presented, based upon the fundamental identity of the components of the interior 82% of the Earth, the endo-Earth, with corresponding components of the Abee enstatite chondrite meteorite. Within limits of existing data, the following generalizations concerning the endo-Earth radionuclides can be made: (1) Most of the K-40 may be expected to exist in combination with oxygen in the silicates of the lower mantle, perhaps being confined to the upper region of the lower mantle where it transitions to the upper mantle; (2) Uranium may be expected to exist at the center of the Earth where it may undergo self-sustaining nuclear fission chain reactions, but there is a possibility that some non-fissioning uranium may be found scattered diffusely within the core floaters…
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Taxonomy
TopicsNeutrino Physics Research · Radioactive contamination and transfer · Quantum, superfluid, helium dynamics
