On the 14C content in radioactive ores

A. J.T. Jull; D. L. Barker; D. J. Donahue

doi:10.1016/0168-9622(87)90026-1

On the ¹⁴C content in radioactive ores

A. J.T. Jull
, D. L. Barker
, D. J. Donahue

Geosciences

Research output: Contribution to journal › Article › peer-review

13 Scopus citations

Abstract

U and Th ores have been found to contain significant levels of ¹⁴C. The levels of this isotope can be as high as ¹⁴C α=1.7 · 10^-9, and can be explained in terms of nuclear reactions and some contribution from heavy-ion emission or asymmetric fission. The levels of ¹⁴C are compared to other nucleogenic isotopes that have been found in these ores, such as ¹⁰Be, ²⁶Al and excesses of rare-gas isotopes.

Original language	English (US)
Pages (from-to)	35-40
Number of pages	6
Journal	Chemical Geology: Isotope Geoscience Section
Volume	66
Issue number	1-2
DOIs	https://doi.org/10.1016/0168-9622(87)90026-1
State	Published - Nov 25 1987

ASJC Scopus subject areas

General Environmental Science
General Earth and Planetary Sciences

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abstract = "U and Th ores have been found to contain significant levels of 14C. The levels of this isotope can be as high as 14C α=1.7 · 10-9, and can be explained in terms of nuclear reactions and some contribution from heavy-ion emission or asymmetric fission. The levels of 14C are compared to other nucleogenic isotopes that have been found in these ores, such as 10Be, 26Al and excesses of rare-gas isotopes.",

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AU - Jull, A. J.T.

AU - Barker, D. L.

AU - Donahue, D. J.

PY - 1987/11/25

Y1 - 1987/11/25

N2 - U and Th ores have been found to contain significant levels of 14C. The levels of this isotope can be as high as 14C α=1.7 · 10-9, and can be explained in terms of nuclear reactions and some contribution from heavy-ion emission or asymmetric fission. The levels of 14C are compared to other nucleogenic isotopes that have been found in these ores, such as 10Be, 26Al and excesses of rare-gas isotopes.

AB - U and Th ores have been found to contain significant levels of 14C. The levels of this isotope can be as high as 14C α=1.7 · 10-9, and can be explained in terms of nuclear reactions and some contribution from heavy-ion emission or asymmetric fission. The levels of 14C are compared to other nucleogenic isotopes that have been found in these ores, such as 10Be, 26Al and excesses of rare-gas isotopes.

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U2 - 10.1016/0168-9622(87)90026-1

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JO - Chemical Geology: Isotope Geoscience Section

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ER -

On the ¹⁴C content in radioactive ores

Abstract

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