
In situ produced 14C by cosmic ray muons in ablating Antarctic ice
Abstract
Samples of a core (52 m) of ablating Antarctic ice were analysed for 14CO and 14CO2 by accelerator mass spectrometry. The data were compared with a 14C in situ production model that includes muon capture in addition to oxygen spallation by neutrons. The analysis reveals significant in situ 14C at depths below 10 m, which we attribute to 14C production by cosmic ray muons. The age of the ice was determined as 9.3±0.4 14C ka BP.
DOI: https://doi.org/10.3402/tellusb.v54i2.16658 | Journal eISSN: 1600-0889
Language: English
Page range: 186 - 192
Submitted on: Dec 28, 2000
Accepted on: Oct 22, 2001
Published on: Jan 1, 2002
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2002 W. J. M. van der Kemp, C. Alderliesten, K. Vander Borg, A. F. M. de Jong, R. A. N. Lamers, J. Oerlemans, M. Thomassen, R. S. W. van de Wal, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.