THE CARBONATE C-14 BACKGROUND AND ITS COMPONENTS AT THE LEIBNIZ AMS FACILITY

Citation
M. Schleicher et al., THE CARBONATE C-14 BACKGROUND AND ITS COMPONENTS AT THE LEIBNIZ AMS FACILITY, Radiocarbon, 40(1), 1998, pp. 85-93
Citations number
9
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
00338222
Volume
40
Issue
1
Year of publication
1998
Part
1
Pages
85 - 93
Database
ISI
SICI code
0033-8222(1998)40:1<85:TCCBAI>2.0.ZU;2-V
Abstract
After routine accelerator mass spectrometry (AMS) radiocarbon dating h ad been established at the Leibniz-Labor with the completion of system s for CO2 production, graphitization, and target making, a systematic investigation was conducted to find the sources of C-14 concentrations observed in background materials. We quantified the contributions of the AMS-system, the reduction, CO2 production from carbonate, carbonat e contamination, and combustion. Carbonate contamination appears to be the dominating factor. Improvements in the pretreatment of foraminife r carbonate have led to the elimination of most of this contamination.