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Geochemical Journal
Geochemical Journal An open access journal for geochemistry
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Micro-determinations of C, N, S, H, He, metallic Fe, δ13C, δ15N and δ34S in geologic samples

H. Sakai, J. W. Smith, I. R. Kaplan, C. Petrowski
Geochemical Journal, Vol. 10, No. 2, P. 85-96, 1976

ABSTRACT

Pyrolysis-combustion, direct combustion and hydrolysis procedures have been developed for study of returned lunar samples. These procedures are also applicable to the analysis of numerous elements on relatively small geological specimens. During pyrolysis-combustion, the sample is degassed at 150°C, heated in vacuum to 1, 225°C and the various gaseous products are measured and collected. Then, the pyrolysis residue is combusted in a partial atmosphere of oxygen and additional gaseous products are collected. The above method allows the following measurements: C (as CO2, CH4 and CO); total H, total He, total N, combusted C, δ13CPDB and δ15Nair. By direct combustion in oxygen, the abundances of C, S, N and He, as well as δ13CPDB, δ15Nair and δ34SCD are determined. Hydrolysis involves reacting the sample in 6N H2SO4 overnight at 105°C. The gaseous products collected and measured are: S (as H2S), δ34SCD, acid hydrolyzable CH4, He and % metallic Fe (from H2 released). Standards were analyzed to demonstrate the capabilities and reliabilities of the different experiments. A suite of lunar samples was studied using these new techniques. Replicate and duplicate analyses of these samples and a comparison with literature values obtained by different methods show a high degree of confidence which can be placed in the techniques described.

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