Thursday, 8 September 2005

This presentation is part of: Poster Session II

A new trial method in the detection of trace elements in quartz samples

Kyeong J. Kim, Dept. Physics, Univ. Arizona, Tucson, AZ 85721, William J. Trompetter, Institute of Geological and Nuclear Sciences, Ltd., 30 Gracefield Road, Lower Hutt, New Zealand, and Chris Eastoe, Department of Geosciences, University of Arizona, Tucson, AZ 85721.

Common metamorphic quartz samples have abundant fluid inclusions that contain C, N, H2O etc. Understanding the nitrogen content in quartz is especially important since neutron capture by nitrogen would contribute a significant amount of the total in situ 14C production in cosmic ray exposed quartz [1]. To determine carbon and nitrogen content experimentally, we applied nuclear reaction analysis (NRA) using a 1.4 MeV deuteron beam [2]. Sample pellets were made with about ~50 mg of each sample. The nuclear reactions 14N(d,α0) and 12C(d,p0) were used to estimate atomic concentrations of N and C, respectively. In our six samples, the range of nitrogen concentration was 0.008 ± 0.001 to 0.050 ± 0.002 at%, and the carbon content ranged from 0.0005 ± 0.0003 to 0.0017 ± 0.0003 at%. The large errors associated with these estimates are due to low counting statistics from measurements of trace concentrations near the limits of detection.

We also used a Costech Elemental Analyzer to determine nitrogen and carbon content. About 100 mg of each sample was heated rapidly to 1030°C, resulting in the decrepitation of fluid inclusions and the release of C and N gaseous species into the He carrier gas. The nitrogen content of the quartz varies from 0.001 to 0.002 wt%, consistent with that of NRA, but with poor precision because measurements are at the limit of detection. The carbon concentrations of our samples ranges from 0.0086 to 0.0242 wt% with better-defined chromatogram peaks than those of nitrogen. The ratios of C/N concentration in the fluid inclusion of quartz from this method are consistent with published results [3]. Further investigation is needed for the development of a reliable method of determination of C and N in quartz samples that could be used for in situ 14C analysis for exposure dating applications.

[1] Lal and Jull, NIM B92 (1994) 291-296; [2] Vickridge et al., NIM B118 (1996) 608-612; [3] de Ronde et al., Econ. Geol. (2000) 1025-1045.


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See more of The 10th International Conference on Accelerator Mass Spectrometry (September 5-10, 2005)