The seasonal location of the core of the Earth — is an important geodynamic factor of the planet

The seasonal location of the core of the Earth — is an important geodynamic factor of the planet

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Дата:2010
Автор: Drevitska, O.
Формат: Стаття
Мова:English
Опубліковано: Інститут геофізики ім. С.I. Субботіна НАН України 2010
Назва видання:Геофизический журнал
Онлайн доступ:http://dspace.nbuv.gov.ua/handle/123456789/101320
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Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Цитувати:The seasonal location of the core of the Earth — is an important geodynamic factor of the planet / O. Drevitska // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 38-39. — Бібліогр.: 6 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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spelling irk-123456789-1013202016-06-03T03:01:55Z The seasonal location of the core of the Earth — is an important geodynamic factor of the planet Drevitska, O. 2010 Article The seasonal location of the core of the Earth — is an important geodynamic factor of the planet / O. Drevitska // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 38-39. — Бібліогр.: 6 назв. — англ. 0203-3100 http://dspace.nbuv.gov.ua/handle/123456789/101320 en Геофизический журнал Інститут геофізики ім. С.I. Субботіна НАН України
institution Digital Library of Periodicals of National Academy of Sciences of Ukraine
collection DSpace DC
language English
format Article
author Drevitska, O.
spellingShingle Drevitska, O.
The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
Геофизический журнал
author_facet Drevitska, O.
author_sort Drevitska, O.
title The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
title_short The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
title_full The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
title_fullStr The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
title_full_unstemmed The seasonal location of the core of the Earth — is an important geodynamic factor of the planet
title_sort seasonal location of the core of the earth — is an important geodynamic factor of the planet
publisher Інститут геофізики ім. С.I. Субботіна НАН України
publishDate 2010
url http://dspace.nbuv.gov.ua/handle/123456789/101320
citation_txt The seasonal location of the core of the Earth — is an important geodynamic factor of the planet / O. Drevitska // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 38-39. — Бібліогр.: 6 назв. — англ.
series Геофизический журнал
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AT drevitskao seasonallocationofthecoreoftheearthisanimportantgeodynamicfactoroftheplanet
first_indexed 2025-07-07T10:44:21Z
last_indexed 2025-07-07T10:44:21Z
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fulltext /#�)-(% '0%.�+,#(� #(%1 �2 ��������� ��� ���������������������� The seasonal location of the core of the Earth — is an important geodynamic factor of the planet O. Drevitska, 2010 National Medical Academy of Postgraduate Education, '��� �� �9 :��� � �9 �;������ Kiev, �;����� ����� ;���;���� The scientific literature is not elaborate enough to consider the importance of the seasonal location of the core of the Earth as a factor of geodynamic processes [Greiner-Mai et al., 2003; Antonov, Kon- dratjev, 2004; Malyshkov Yu., Malyshkov S., 2009]. In our work we present a logical rational of the con- cept. The first position. Newton's second law of the force of gravity states that there is a direct propor- tional relation to the mass of bodies and inversely proportional to the distance between them. Weight is calculated as the product of the specific body weight and its volume. The core of the Earth has a larger proportion (this fact is proved by numerous gravimetric studies) [http://uk.wikipedia.org/wiki/ Geophysic]. It is known that the Earth's core consists of 90% iron while the mantle contains of only 10 % iron and a proportion of the other elements — oxygen, silicon and magnesium [Allegre et al., 1995]. Therefore, the force of gravity per unit volume of Earth's core is higher and the nucleus constantly presses the inside the mantle. Pressure is directed towards the Sun and as the Earth rotates the con- stantly changing area of highest pressure is inside the kernel. So, the Earth's core is heavier, and in accor- dance with Newton's second law, more attracted to the sun. This is partly accounted for in the scienti- fic literature. The second position. The axis of the Earth is tilted 23 degrees to the ecliptic plane. Earth is fa- cing the Sun at an angle, in the summer inside the nucleus at an angle of more pressure on the nor- thern hemisphere, and in the winter — on the Sou- thern. Findings from the provisions of 1 and 2. The core of the Earth not only rotates inside the planet, but also seasonally shifts to the Northern Hemisphere and then to the Southern, as shown in the picture (Figure). In the presented picture (when the Earth is right) shows how the Earth's core is offset at an angle of 23 degrees in the direction of the Northern Hemi- sphere, when we have the summer season. Inside — the pressure on the mantle. The pic- ture also shows (when the Earth is on the left) as the core is offset at an angle to the Southern Hemi- sphere, when we have the winter season. Such internal displacement of the Earth's core (as conventionally shown "on the cut") reaches its highest value in the following periods: December— January and June—July. The pressure inside the kernel, its friction and seasonal shifts significantly affects: earthquakes and volcanoes, the movement of continents and the forma- tion of mountain ranges, the formation of plumes, subduction, nuta- tion, and other geodynamic processes. During the summer, forming elevations in the Northern Hemisphere, are active volcanoes, earth- quakes that occur in the projections of the nucleus and the more pressure field "breaks" of tectonic ��������� ��� ���������������������� �3 ��� ��!"#�$%&'�("�%()�#*+#�' #(&"�&��&,#��-�%()� �)#..'(/ plates. Seasonal shift in the Earth's core could ex- plain the gaps of tectonic plates and their move- ment. During our winter season, shaped elevations in the Southern Hemisphere are active volcanoes, earth- quakes occur in the relatively "weak" field. In the nor- thern hemisphere, meanwhile, it may also occur from an earthquake, but the land, that "sinks", hence an understanding for the reasons for subduction. Seasonal location of the core of the Earth is im- portant geodynamic effects, as evidenced by the presence of zones of high tectonic activnosi on both sides of the equator. This increases the tectonic activity in the Southern Hemisphere in December— January, and in the Northern — in June and July. The core of the Earth — it is almost a "perpetual motion" inside the planet until there is a structure of the Earth's axis and the trajectory of the Earth around the Sun. This concept should be considered when crea- ting a computer model of the Earth, a view of the seasonal movement of the nucleus, in order to bet- ter predict those processes that will occur inside and on the surface of our planet. References A l l e g r e C . J . , P o i r i e r J . P. , H u m l e r E . , Hofmann A. W. The Chemical-Composition of the Earth // Earth Planet. Sci. Lett. — 1995. — 134(3-4). — P. 515—526. Antonov V. A., Kondratjev B. P. On the problem of the value of the interior Earth’s core displacement ++ &�� � ��� �� � 0 366,� 0 �)),� 0 ��)).*0.. <�� %� ���=� Greiner-Mai H., Jochmann H., Barthelmes F., Ballani L. Possible infleunces of core processes on the Earth’s rotation and the gravity field // J. Geo- dynam. — 2003. — 36� �))*� 0 ��))343—358. http://www.izdatgeo.ru http://uk.wikipedia.org/wiki/Geophysic Malyshkov Yu. P., Malyshkov S. Yu. Periodic varia- tions of geophysical fields and seismic activity, their possible connection with the Earth’s core motions // Geology and Geophysics. — 2009. — 50� �))3� 0 ��))/-30/73 (in Russian).

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