The 21Ne production rate in stony meteorites estimated from 10Be and other radionuclides
Document Type
Article
Publication Date
1-1-1983
Abstract
The 10Be contents of 28 stony meteorites with known 21Ne contents range from 0.97 to 23 dpm/kg and give an average 21Ne production rate (P21) of (0.28 ± 0.02) × 108 cm3 STP/g-Myr for shielding conditions corresponding to 22Ne 21Ne = 1.114 in an H-chondrite. Our P21(10Be) agrees with others' P21 based on 22Na, 81Kr and 53Mn but not on 26A1. Temporal variations in the cosmic ray flux do not explain the disagreement satisfactorily; major errors in the radionuclide half-lives are not indicated. The discrepancy seems rooted in the data selection and the difficulties of making accurate corrections for shielding, chemical composition and other sources of variability. © 1983.
Identifier
0020916787 (Scopus)
Publication Title
Geochimica Et Cosmochimica Acta
External Full Text Location
https://doi.org/10.1016/0016-7037(83)90205-3
ISSN
00167037
First Page
1887
Last Page
1895
Issue
11
Volume
47
Recommended Citation
Moniot, R. K.; Kruse, T. H.; Tuniz, C.; Savin, W.; Hall, G. S.; Milazzo, T.; Pal, D.; and Herzog, G. F., "The 21Ne production rate in stony meteorites estimated from 10Be and other radionuclides" (1983). Faculty Publications. 21314.
https://digitalcommons.njit.edu/fac_pubs/21314
