Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core

The description problem of geoantineutrino spectrum and reactor antineutrino experimental spectrum in KamLAND, which takes place for antineutrino energy ~ 2.8 MeV, and also the experimental results of the interaction of uranium dioxide and carbide with iron-nickel and silica-alumina melts at high pr...

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Veröffentlicht in:Український антарктичний журнал
Datum:2006
Hauptverfasser: Rusov, V.D., Pavlovich, V.N., Vaschenko, V.N., Tarasov, V.A., Zelentsova, T.N., Bolshakov, V.N., Litvinov, D.A., Kosenko, S.I., Byegunova, O.A.
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Sprache:Englisch
Veröffentlicht: Національний антарктичний науковий центр МОН України 2006
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Online Zugang:https://nasplib.isofts.kiev.ua/handle/123456789/128263
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Zitieren:Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core / V.D. Rusov, V.N. Pavlovich, V.N. Vaschenko, V.A. Tarasov, T.N. Zelentsova, V.N. Bolshakov, D.A. Litvinov, S.I. Kosenko, O.A. Byegunova // Український антарктичний журнал. — 2006. — № 4-5. — С. 182-202. — Бібліогр.: 63 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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author Rusov, V.D.
Pavlovich, V.N.
Vaschenko, V.N.
Tarasov, V.A.
Zelentsova, T.N.
Bolshakov, V.N.
Litvinov, D.A.
Kosenko, S.I.
Byegunova, O.A.
author_facet Rusov, V.D.
Pavlovich, V.N.
Vaschenko, V.N.
Tarasov, V.A.
Zelentsova, T.N.
Bolshakov, V.N.
Litvinov, D.A.
Kosenko, S.I.
Byegunova, O.A.
citation_txt Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core / V.D. Rusov, V.N. Pavlovich, V.N. Vaschenko, V.A. Tarasov, T.N. Zelentsova, V.N. Bolshakov, D.A. Litvinov, S.I. Kosenko, O.A. Byegunova // Український антарктичний журнал. — 2006. — № 4-5. — С. 182-202. — Бібліогр.: 63 назв. — англ.
collection DSpace DC
container_title Український антарктичний журнал
description The description problem of geoantineutrino spectrum and reactor antineutrino experimental spectrum in KamLAND, which takes place for antineutrino energy ~ 2.8 MeV, and also the experimental results of the interaction of uranium dioxide and carbide with iron-nickel and silica-alumina melts at high pressure (5-10 GPа) and temperature (1600-2200°C) have motivated us to consider the possible consequences of the assumption made by V.Anisichkin and coauthors that there is an actinid shell on boundary of liquid and solid phases of the Earth's core. We have shown that the activation of a natural nuclear reactor operating as the solitary waves of nuclear burning in ²³⁸U- and/or ²³²Th-medium (in particular, the neutron-fission progressive wave of Feoktistov and/or Teller-Ishikawa-Wood) can be such a physical consequence. The simplified model of the kinetics of accumulation and burnup in U-Pu fuel cycle of Feoktistov is developed. The results of the numerical simulation of neutron-fission wave in two-phase UO₂/Fe medium on a surface of the Earth's solid core are presented. The georeactor model of 3He origin and the ³He/⁴He-ratio distribution in the Earth’s interior is offered. It is shown that the ³He/⁴He ratio distribution can be the natural quantitative criterion of georeactor thermal power. On the basis of O'Nions-Evensen-Hamilton geochemical model of mantle differentiation and the crust growth supplied by actinid shell on the boundary of liquid and solid phases of the Earth's core as a nuclear energy source (georeactor with power of 30 TW), the tentative estimation of geoantineutrino intensity and geoantineutrino spectrum on the Earth surface are given.
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last_indexed 2025-12-07T19:32:49Z
publishDate 2006
publisher Національний антарктичний науковий центр МОН України
record_format dspace
spelling Rusov, V.D.
Pavlovich, V.N.
Vaschenko, V.N.
Tarasov, V.A.
Zelentsova, T.N.
Bolshakov, V.N.
Litvinov, D.A.
Kosenko, S.I.
Byegunova, O.A.
2018-01-07T15:42:48Z
2018-01-07T15:42:48Z
2006
Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core / V.D. Rusov, V.N. Pavlovich, V.N. Vaschenko, V.A. Tarasov, T.N. Zelentsova, V.N. Bolshakov, D.A. Litvinov, S.I. Kosenko, O.A. Byegunova // Український антарктичний журнал. — 2006. — № 4-5. — С. 182-202. — Бібліогр.: 63 назв. — англ.
1727-7485
https://nasplib.isofts.kiev.ua/handle/123456789/128263
The description problem of geoantineutrino spectrum and reactor antineutrino experimental spectrum in KamLAND, which takes place for antineutrino energy ~ 2.8 MeV, and also the experimental results of the interaction of uranium dioxide and carbide with iron-nickel and silica-alumina melts at high pressure (5-10 GPа) and temperature (1600-2200°C) have motivated us to consider the possible consequences of the assumption made by V.Anisichkin and coauthors that there is an actinid shell on boundary of liquid and solid phases of the Earth's core. We have shown that the activation of a natural nuclear reactor operating as the solitary waves of nuclear burning in ²³⁸U- and/or ²³²Th-medium (in particular, the neutron-fission progressive wave of Feoktistov and/or Teller-Ishikawa-Wood) can be such a physical consequence. The simplified model of the kinetics of accumulation and burnup in U-Pu fuel cycle of Feoktistov is developed. The results of the numerical simulation of neutron-fission wave in two-phase UO₂/Fe medium on a surface of the Earth's solid core are presented. The georeactor model of 3He origin and the ³He/⁴He-ratio distribution in the Earth’s interior is offered. It is shown that the ³He/⁴He ratio distribution can be the natural quantitative criterion of georeactor thermal power. On the basis of O'Nions-Evensen-Hamilton geochemical model of mantle differentiation and the crust growth supplied by actinid shell on the boundary of liquid and solid phases of the Earth's core as a nuclear energy source (georeactor with power of 30 TW), the tentative estimation of geoantineutrino intensity and geoantineutrino spectrum on the Earth surface are given.
en
Національний антарктичний науковий центр МОН України
Український антарктичний журнал
Ядерно-фізичні дослідження Землі та атмосфери
Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
Article
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spellingShingle Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
Rusov, V.D.
Pavlovich, V.N.
Vaschenko, V.N.
Tarasov, V.A.
Zelentsova, T.N.
Bolshakov, V.N.
Litvinov, D.A.
Kosenko, S.I.
Byegunova, O.A.
Ядерно-фізичні дослідження Землі та атмосфери
title Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
title_full Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
title_fullStr Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
title_full_unstemmed Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
title_short Geoantineutrino Spectrum, ³He/⁴He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning of the Liquid and Solid Phases of the Earth's Core
title_sort geoantineutrino spectrum, ³he/⁴he-ratio distribution in the earth's interior and slow nuclear burning of the liquid and solid phases of the earth's core
topic Ядерно-фізичні дослідження Землі та атмосфери
topic_facet Ядерно-фізичні дослідження Землі та атмосфери
url https://nasplib.isofts.kiev.ua/handle/123456789/128263
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