Elemental Abundances of Ultraheavy Cosmic Rays
Abstract
The elemental composition of the cosmic-ray source is different from that which has been generally taken as the composition of the solar system. No general enrichment of products of either r-process or s-process nucleosynthesis accounts for the differences over the entire range of ultraheavy (Z > 30) elements; specific determination of nucleosynthetic contributions to the differences depends upon an understanding of the nature of any acceleration fractionation. Comparison between the cosmic-ray source abundances and the abundances of C1 and C2 chondritic meteorites suggests the possibility that differences between the cosmic-ray source and the "standard (C1) solar system" may not be due to acceleration fractionation of the cosmic rays, but may be due instead to a fractionation of the C1 abundances with respect to the interstellar abundances.
Additional Information
Copyright © 1984 Elsevier. This work was supported in part by NASA under contracts NAS8-27976, 77, 78 and grants NGR 005-002-160, 24-005-050, 26-008-001.Additional details
- Eprint ID
- 45274
- DOI
- 10.1016/0273-1177(84)90289-8
- Resolver ID
- CaltechAUTHORS:20140429-095757981
- NASA
- NAS8-27976
- NASA
- NAS8-27977
- NASA
- NAS8-27978
- NASA
- NGR 05-002-160
- NASA
- NGR 24-005-050
- NASA
- NGR 26-008-001
- Created
-
2014-04-30Created from EPrint's datestamp field
- Updated
-
2021-11-10Created from EPrint's last_modified field
- Caltech groups
- Space Radiation Laboratory
- Other Numbering System Name
- Space Radiation Laboratory
- Other Numbering System Identifier
- 1984-02