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Agyei, E. K., McMullen, C. C. (1968) A study of the isotopic abundance of boron from various sources. Canadian Journal of Earth Sciences, 5 (4) 921-927 doi:10.1139/e68-088

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Reference TypeJournal (article/letter/editorial)
TitleA study of the isotopic abundance of boron from various sources
JournalCanadian Journal of Earth Sciences
AuthorsAgyei, E. K.Author
McMullen, C. C.Author
Year1968 (August 1)Volume5
Page(s)921-927Issue4
PublisherCanadian Science Publishing
DOIdoi:10.1139/e68-088Search in ResearchGate
Mindat Ref. ID472042Long-form Identifiermindat:1:5:472042:7
GUID173b3eb3-5dd4-438a-97c3-d0e72970f6e0
Full ReferenceAgyei, E. K., McMullen, C. C. (1968) A study of the isotopic abundance of boron from various sources. Canadian Journal of Earth Sciences, 5 (4) 921-927 doi:10.1139/e68-088
Plain TextAgyei, E. K., McMullen, C. C. (1968) A study of the isotopic abundance of boron from various sources. Canadian Journal of Earth Sciences, 5 (4) 921-927 doi:10.1139/e68-088
In(1968, August) Canadian Journal of Earth Sciences Vol. 5 (4) Canadian Science Publishing
Abstract/Notes The absolute ratio of 11B/10B has been determined for boron from different terrestrial sources with a precision of 0.2% (two standard errors) and a reproducibility of 0.2% (half-range). Values fall in the range 4.108 to 3.987 (i.e. 3% variation) and give a corresponding range in the boron atomic weight of 10.814 to 10.810 (0.04% variation). The absolute ratios are 7% lower than those reported by early workers, but are in accord with the results of recent investigations. Igneous rocks and boric acid are found to have high isotopic ratios, whereas Tokyo Bay water possesses a value for 11B/10B near the mean.


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