A Fairy Tale of Identical Nuclides That Can Exchange Nucleons

Under the assumption that identical nuclides, when brought very close to each other at the minimum possible distance for a relatively long time, can exchange nucleons with the preservation of their total number and the release of excess energy, it is shown that some of the nuclides formed in this case cannot enter into such reactions, i.e. they can be considered as spent fuel. An analysis of the isotopic composition of the earth's crust showed that more than 85% of thenuclides in the earth's crust are spent fuel. It is suggested that similar nuclear reactions with a gradual accumulation of spent fuel took place in the bowels of the Earth, which ultimately led to a decrease in their intensity, a decrease in temperature and the formation of a solidified crust. Arguments are given in favor of the fact that similar reactions continue in the bowels of the Earth at the present time. It is assumed that the appearance of heavy elements in the earth's crust, the presence of an additional heat source ensuring the thermal balance of the Earth, and the relatively young age of uranium U238 in the earth's crust may also be the result of similar reactions.

Authors

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-02-16
DOI
https://doi.org/10.5281/zenodo.18662867
Primary Topic
Cold Fusion and Nuclear Reactions
Type
article
Field-Weighted Citation Impact
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article

A Fairy Tale of Identical Nuclides That Can Exchange Nucleons

V. P. Torchigin
Zenodo (CERN European Organization for Nuclear Research)
Cold Fusion and Nuclear Reactions
article

A Fairy Tale of Identical Nuclides That Can Exchange Nucleons

V. P. Torchigin
article en

Abstract

Under the assumption that identical nuclides, when brought very close to each other at the minimum possible distance for a relatively long time, can exchange nucleons with the preservation of their total number and the release of excess energy, it is shown that some of the nuclides formed in this case cannot enter into such reactions, i.e. they can be considered as spent fuel. An analysis of the isotopic composition of the earth's crust showed that more than 85% of thenuclides in the earth's crust are spent fuel. It is suggested that similar nuclear reactions with a gradual accumulation of spent fuel took place in the bowels of the Earth, which ultimately led to a decrease in their intensity, a decrease in temperature and the formation of a solidified crust. Arguments are given in favor of the fact that similar reactions continue in the bowels of the Earth at the present time. It is assumed that the appearance of heavy elements in the earth's crust, the presence of an additional heat source ensuring the thermal balance of the Earth, and the relatively young age of uranium U238 in the earth's crust may also be the result of similar reactions.

Zenodo (CERN European Organization for Nuclear Research)
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