In-Situ Radiocarbon Production by Neutrons and Muons in an Antarctic Blue Ice Field at Scharffenbergbotnen: A Status Report

In the radiocarbon accelerator mass spectrometry ( 14 C AMS) analysis of gases obtained in a dry extraction from a 52–m Antarctic ice core, we observed 14 CO 2 and 14 CO concentrations decreasing with depth. The concentrations are explained in terms of in-situ production by neutrons and captured muo...

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Bibliographic Details
Published in:Radiocarbon
Main Authors: van der Borg, K, van der Kemp, W J M, Alderliesten, C, de Jong, A F M, Lamers, R A N, Oerlemans, J, Thomassen, M, van de Wal, R S W
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2001
Subjects:
Antarc*
Antarctic
ice core
Online Access:http://dx.doi.org/10.1017/s0033822200041412
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200041412
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Summary:In the radiocarbon accelerator mass spectrometry ( 14 C AMS) analysis of gases obtained in a dry extraction from a 52–m Antarctic ice core, we observed 14 CO 2 and 14 CO concentrations decreasing with depth. The concentrations are explained in terms of in-situ production by neutrons and captured muons in ablating ice. The ratio of the 14 CO2 concentration to that of 14 CO has been found to be constant at 1.9 ± 0.3. The ablation rates obtained of 42 ± 18 cm.yr −1 and 40 ± 13 cm.yr −1 for the neutron and muon components, respectively, are about three times higher than observed from stake readings. The discrepancy may point to an incomplete extraction of the dry extraction method. Using the constant ratio in 14 CO 2 and 14 CO concentrations we correct for the in-situ component in the trapped 14 CO 2 and deduce an age of 10,300 ± 900 BP for the ice core.

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