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Neftyanaya Provintsiya 
No.1(29),2022

Deep Degassing as a Temperature Factor on the Earth Atmosphere

V.L. Syvorotkin

DOI: https://doi.org/10.25689/NP.2022.1.33-48

PP.33-48

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Abstract
References

Abstract

I suppose the main claims to the global hydrocarbon energy sector made by the Paris Climate Agreement of 2015 are not substantiated. The real cause of modern climate change dwells on the planetary intensive process of the hydrogen degassing which generates a complex of physico-chemical effects emitting heat.

1 - negative throttling effect, i.e. the very release of hydrogen on the daytime surface leads to heating of the surface air.

2 - exothermic oxidation of hydrogen and methane in the atmosphere.

3 - the air ionization effect by radioactive gases released from the ground together with hydrogen lead to condensation of water vapor with the heat release.

4- the destruction of the ozone layer causes an increase in the flow of ultraviolet light to the Earth's surface, which, in turn, triggers ozone-forming reactions. The ground-level ozone increases by 2-3 times, the decay of its molecules occurs with the release of thermal radiation.

Key words:

Paris Agreement, climate change, hydrogen degassing, choke effect, hydrogen oxidation, air ionization, ozone layer destruction, ground-level ozone

References

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Authors

V.L. Syvorotkin, D.Sc. (Geology and Mineralogy) Geological Department Lomonosov Moscow State University, Leading Researcher, Honored Researcher MSU, Full Member of the Russian Academy of Natural Sciences

ID – ORCID htpps://orcid.org/0000-0003-2846-8484

1, Leninskie gory, GSP-1, Moscow, 119234, Russian Federation

E-mail: hlozon@mail.ru

For citation:

V.L. Syvorotkin Glubinnaja degazacija zemli kak faktor temperaturnogo vozdejstvija na atmosferu [Deep Degassing as a Temperature Factor on the Earth Atmosphere]. Neftyanaya Provintsiya, No. 1(29), 2022. pp. 33-48. DOI https://doi.org/10.25689/NP.2022.1.33-48 (in Russian)

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   © V.L. Syvorotkin, 2022
       This is an open access article under the Creative Commons Attribution 4.0 License (https://creativecommons.org/licenses/by/4.0/)

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