Progress in 14C dating of ice at Utrecht

For 14C dating of ice, only a limitad amount of CO2 is available (20-100 mg C/kg ice). To avoid contamination, a special miling device has been constructed to chip the ice at -20°C. The background of 7.0 +/- 2.0 percent modern carbon (pmC) for a sample of 50 mgC, including extraction and conversion,...

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Main Authors: van de Wal, R. S. W., van der Borg, K., Oerter, Hans, Reeh, N., Jong, A. F. M. de, Oerlemans, J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1990
Subjects:
Online Access:https://epic.awi.de/id/eprint/3248/
https://hdl.handle.net/10013/epic.13831
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spelling ftawi:oai:epic.awi.de:3248 2023-09-05T13:19:51+02:00 Progress in 14C dating of ice at Utrecht van de Wal, R. S. W. van der Borg, K. Oerter, Hans Reeh, N. Jong, A. F. M. de Oerlemans, J. 1990 https://epic.awi.de/id/eprint/3248/ https://hdl.handle.net/10013/epic.13831 unknown van de Wal, R. S. W. , van der Borg, K. , Oerter, H. , Reeh, N. , Jong, A. F. M. d. and Oerlemans, J. (1990) Progress in 14C dating of ice at Utrecht , Nuclear instruments and methods in physics research, B52, pp. 469-472 . hdl:10013/epic.13831 EPIC3Nuclear instruments and methods in physics research, B52, pp. 469-472 Article isiRev 1990 ftawi 2023-08-22T19:43:55Z For 14C dating of ice, only a limitad amount of CO2 is available (20-100 mg C/kg ice). To avoid contamination, a special miling device has been constructed to chip the ice at -20°C. The background of 7.0 +/- 2.0 percent modern carbon (pmC) for a sample of 50 mgC, including extraction and conversion, limits the 14C dating of ice with accelerator mass spectroscopy (AMS) to about 20 000 years B.P. Results are presented for an ice core from the Pakitsoq area, West Greenland, with a known age of 9000 +/- 1000 years B.P., established by means of delta-18O variations and ice flow model calculations. Article in Journal/Newspaper Greenland ice core Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Greenland
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description For 14C dating of ice, only a limitad amount of CO2 is available (20-100 mg C/kg ice). To avoid contamination, a special miling device has been constructed to chip the ice at -20°C. The background of 7.0 +/- 2.0 percent modern carbon (pmC) for a sample of 50 mgC, including extraction and conversion, limits the 14C dating of ice with accelerator mass spectroscopy (AMS) to about 20 000 years B.P. Results are presented for an ice core from the Pakitsoq area, West Greenland, with a known age of 9000 +/- 1000 years B.P., established by means of delta-18O variations and ice flow model calculations.
format Article in Journal/Newspaper
author van de Wal, R. S. W.
van der Borg, K.
Oerter, Hans
Reeh, N.
Jong, A. F. M. de
Oerlemans, J.
spellingShingle van de Wal, R. S. W.
van der Borg, K.
Oerter, Hans
Reeh, N.
Jong, A. F. M. de
Oerlemans, J.
Progress in 14C dating of ice at Utrecht
author_facet van de Wal, R. S. W.
van der Borg, K.
Oerter, Hans
Reeh, N.
Jong, A. F. M. de
Oerlemans, J.
author_sort van de Wal, R. S. W.
title Progress in 14C dating of ice at Utrecht
title_short Progress in 14C dating of ice at Utrecht
title_full Progress in 14C dating of ice at Utrecht
title_fullStr Progress in 14C dating of ice at Utrecht
title_full_unstemmed Progress in 14C dating of ice at Utrecht
title_sort progress in 14c dating of ice at utrecht
publishDate 1990
url https://epic.awi.de/id/eprint/3248/
https://hdl.handle.net/10013/epic.13831
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
genre_facet Greenland
ice core
op_source EPIC3Nuclear instruments and methods in physics research, B52, pp. 469-472
op_relation van de Wal, R. S. W. , van der Borg, K. , Oerter, H. , Reeh, N. , Jong, A. F. M. d. and Oerlemans, J. (1990) Progress in 14C dating of ice at Utrecht , Nuclear instruments and methods in physics research, B52, pp. 469-472 . hdl:10013/epic.13831
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