Motion of a Planet with a Complex Structure
The motion of a planet consisting of a mantle and a core (solid bodies) connected by a viscoelastic layer and interacting with each other and an external point mass by the law of gravitation is considered. The mutual motions of the core and mantle are investigated assuming that the centers of mass o...
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Veröffentlicht in: | Cosmic research 2004-07, Vol.42 (4), p.374-381 |
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description | The motion of a planet consisting of a mantle and a core (solid bodies) connected by a viscoelastic layer and interacting with each other and an external point mass by the law of gravitation is considered. The mutual motions of the core and mantle are investigated assuming that the centers of mass of the planet and external point mass moves along undisturbed Keplerian orbits around the common center of mass of the system. The planetary core and mantle have an axial symmetry and different principal moments of inertia, which leads to a displacement of the center of mantle relative to the center of core and to their mutual rotations. The results obtained on the basis of averaged equations are illustrated by the example of the Earth-Moon system. |
doi_str_mv | 10.1023/B:COSM.0000039737.94955.08 |
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The mutual motions of the core and mantle are investigated assuming that the centers of mass of the planet and external point mass moves along undisturbed Keplerian orbits around the common center of mass of the system. The planetary core and mantle have an axial symmetry and different principal moments of inertia, which leads to a displacement of the center of mantle relative to the center of core and to their mutual rotations. 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The mutual motions of the core and mantle are investigated assuming that the centers of mass of the planet and external point mass moves along undisturbed Keplerian orbits around the common center of mass of the system. The planetary core and mantle have an axial symmetry and different principal moments of inertia, which leads to a displacement of the center of mantle relative to the center of core and to their mutual rotations. The results obtained on the basis of averaged equations are illustrated by the example of the Earth-Moon system.</description><subject>Center of mass</subject><subject>Earth-Moon system</subject><subject>Gravitation</subject><subject>Mantle</subject><subject>Mathematical analysis</subject><subject>Moments of inertia</subject><subject>Orbits</subject><subject>Planets</subject><issn>0010-9525</issn><issn>1608-3075</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNp9kFtLwzAUgIMoOKf_oexFQVqTprntzRVvsDFh-hzSNMGObplJy_TfmzpB8MHzcA4HPs7lA2CCYIZgjm9m03K5WmRwCCwYZpkoBCEZ5EdghCjkKYaMHIMRhAimguTkFJyFsI54pOkIXC9c17ht4myikudWbU2X7JvuLXal2-xa85GsOt_rrvfmHJxY1QZz8VPH4PX-7qV8TOfLh6fydp7qXNAu5RqzHNVWcVUJFXcKa5GoGa0RgVTZSqFCIVUUVR2P44raCudaQ6opwoYpPAaXh7k77957Ezq5aYI27XCd64MUkAmBeZFH8upfElGGMEYs5jGY_EHXrvfb-IfkTFBOCMQRmh4g7V0I3li5881G-U-JoByEy5kchMtf4fJbuIQcfwHVsnI5</recordid><startdate>20040701</startdate><enddate>20040701</enddate><creator>Vil&aposke, VG</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope></search><sort><creationdate>20040701</creationdate><title>Motion of a Planet with a Complex Structure</title><author>Vil&aposke, VG</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c296t-8c3721dfa8ab9a9529ff19d76d1506afba14a1a44bd3078a6fb32cc06c613e7a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Center of mass</topic><topic>Earth-Moon system</topic><topic>Gravitation</topic><topic>Mantle</topic><topic>Mathematical analysis</topic><topic>Moments of inertia</topic><topic>Orbits</topic><topic>Planets</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vil&aposke, VG</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Cosmic research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vil&aposke, VG</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Motion of a Planet with a Complex Structure</atitle><jtitle>Cosmic research</jtitle><date>2004-07-01</date><risdate>2004</risdate><volume>42</volume><issue>4</issue><spage>374</spage><epage>381</epage><pages>374-381</pages><issn>0010-9525</issn><eissn>1608-3075</eissn><abstract>The motion of a planet consisting of a mantle and a core (solid bodies) connected by a viscoelastic layer and interacting with each other and an external point mass by the law of gravitation is considered. The mutual motions of the core and mantle are investigated assuming that the centers of mass of the planet and external point mass moves along undisturbed Keplerian orbits around the common center of mass of the system. The planetary core and mantle have an axial symmetry and different principal moments of inertia, which leads to a displacement of the center of mantle relative to the center of core and to their mutual rotations. The results obtained on the basis of averaged equations are illustrated by the example of the Earth-Moon system.</abstract><cop>New York</cop><pub>Springer Nature B.V</pub><doi>10.1023/B:COSM.0000039737.94955.08</doi><tpages>8</tpages></addata></record> |
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subjects | Center of mass Earth-Moon system Gravitation Mantle Mathematical analysis Moments of inertia Orbits Planets |
title | Motion of a Planet with a Complex Structure |
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