FROM C-14/C-12 MEASUREMENTS TOWARDS RADIOCARBON DATING OF ICE

被引：10

作者：

VANDEWAL, RSW

VANROIJEN, JJ

RAYNAUD, D

VANDERBORG, K

DEJONG, AFM

OERLEMANS, J

LIPENKOV, V

HUYBRECHTS, P

机构：

[1] Institute for Marine and Atmospheric research Utrecht, University of Utrecht, Utrecht, 3584 CC

[2] Robert J. Van de Graaff Laboratorium, University of Utrecht, Utrecht, 3584 CC

[3] Laboratoire de Glaciologie et Géophysique de l'environnement, St Martin D'Hères, 38402

[4] Geografisch Instituut, Vrije Universiteit Brussel, Brussels, B-1050

来源：

TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 1994年 / 46卷 / 02期

关键词：

D O I：

10.1034/j.1600-0889.1994.t01-1-00002.x

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

A dry extraction method of CO2 included in glacier ice adds a contamination equivalent to 1.8 mug modem carbon for a 35 mug C sample. This enables radiocarbon dating by accelerator mass spectrometry of 35 mug C samples to about 25 000 BP. Measured C-14/C-12 ratios are presented for a part of the Vostok ice core, and for some surface samples; high C-14/C-12 values ranging between 65 and 105 pm C indicate in-situ C-14 production during the ablation. The reproducibility of radiocarbon dating of ice is demonstrated by results for some parts of the Caroline core, yielding an age versus depth profile, in which the age does not simply increases with depth. The results indicate that the accuracy of radiocarbon dating of ice is not limited by the statistical error arising in the accelerator measurements, but by the uncertainty in the contamination background of the samples and by the in-situ production of C-14.

引用

页码：94 / 102

页数：9