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Aluminum-26 as a planetoid heat source in the early solar systemThe results of thermal model calculations which assume Al-26 as a heat source are presented. The relation between Al-26 content, the maximum central temperature obtained, and the time interval after formation until central cooling commences is elucidated. Because of the heating times required, these results constrain maximum permissible planetoid dimensions more severely than do previous calculations which assume a high initial temperature.
Document ID
19780038315
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Herndon, J. M.
(California, University La Jolla, Calif., United States)
Herndon, M. A.
(San Diego State University San Diego, Calif., United States)
Date Acquired
August 9, 2013
Publication Date
December 31, 1977
Publication Information
Publication: Meteoritics
Volume: 12
Subject Category
Lunar And Planetary Exploration
Accession Number
78A22224
Funding Number(s)
CONTRACT_GRANT: NGL-05-009-005
Distribution Limits
Public
Copyright
Other

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