Kinematic-gravity model of geodynamo
Based on the results of solving the inverse problem of magnetometry and analysis of some known models of the Earth magnetic field generation a model is proposed in which the current producing magnetic field is the vortex motion of positively charged plasma of the planet external core. The main gener...
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| Datum: | 2013 |
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| Format: | Artikel |
| Sprache: | Russisch |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2013
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| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/111381 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543179089641472 |
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| author | Kochnev, V.A. |
| author_facet | Kochnev, V.A. |
| author_sort | Kochnev, V.A. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T12:00:28Z |
| description | Based on the results of solving the inverse problem of magnetometry and analysis of some known models of the Earth magnetic field generation a model is proposed in which the current producing magnetic field is the vortex motion of positively charged plasma of the planet external core. The main generators of the liquid motion are axial rotation of the planet and horizontal components of gravity field of the Moon and the Sun producing on the surface of the planet short-term periodic tides and stabile trade-wind sea currents in the equatorial ocean areas, and the deep currents of ionized liquid in the core. For checking the assumptions mathematical kinematic-gravity model of calculating relative parameters for evaluation of magnetic moment of the planet and magnetic field on the equator has been plotted. The main arguments for calculations are the period of planets rotations, mass and radius of satellites orbits producing the tide forces. For all the planets of the solar system the table of initial and calculated parameters and parameters – results of satellite observations of magnetic field has been given. The coefficient of correlation of calculated and satellite data is 0.997. The conclusion has been made on the close relation of kinematic gravity parameters with parameters of the planets magnetic field. |
| first_indexed | 2025-07-17T11:05:59Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-111381 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:59Z |
| publishDate | 2013 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1113812020-10-07T12:00:28Z Kinematic-gravity model of geodynamo Kochnev, V.A. Based on the results of solving the inverse problem of magnetometry and analysis of some known models of the Earth magnetic field generation a model is proposed in which the current producing magnetic field is the vortex motion of positively charged plasma of the planet external core. The main generators of the liquid motion are axial rotation of the planet and horizontal components of gravity field of the Moon and the Sun producing on the surface of the planet short-term periodic tides and stabile trade-wind sea currents in the equatorial ocean areas, and the deep currents of ionized liquid in the core. For checking the assumptions mathematical kinematic-gravity model of calculating relative parameters for evaluation of magnetic moment of the planet and magnetic field on the equator has been plotted. The main arguments for calculations are the period of planets rotations, mass and radius of satellites orbits producing the tide forces. For all the planets of the solar system the table of initial and calculated parameters and parameters – results of satellite observations of magnetic field has been given. The coefficient of correlation of calculated and satellite data is 0.997. The conclusion has been made on the close relation of kinematic gravity parameters with parameters of the planets magnetic field. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111381 10.24028/gzh.0203-3100.v35i4.2013.111381 Geofizicheskiy Zhurnal; Vol. 35 No. 4 (2013); 3-15 Геофизический журнал; Том 35 № 4 (2013); 3-15 Геофізичний журнал; Том 35 № 4 (2013); 3-15 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111381/106396 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Kochnev, V.A. Kinematic-gravity model of geodynamo |
| title | Kinematic-gravity model of geodynamo |
| title_full | Kinematic-gravity model of geodynamo |
| title_fullStr | Kinematic-gravity model of geodynamo |
| title_full_unstemmed | Kinematic-gravity model of geodynamo |
| title_short | Kinematic-gravity model of geodynamo |
| title_sort | kinematic-gravity model of geodynamo |
| url | https://journals.uran.ua/geofizicheskiy/article/view/111381 |
| work_keys_str_mv | AT kochnevva kinematicgravitymodelofgeodynamo |