Volatile compounds of sulfur in the Fe-C-S system at 5.3 GPa and 1300°C

This report presents the results of experimental studies of the fluid phase in the Fe-C-S system at high P and T values (5.3 GPa and 1300°C) conforming to diamond synthesis. The samples for experiments were mounted on air; therefore, the volatile compounds detected after the experiments are characte...

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Veröffentlicht in:Doklady earth sciences 2015-05, Vol.462 (1), p.527-532
Hauptverfasser: Zhimulev, E. I., Sonin, V. M., Bul’bak, T. A., Chepurov, A. I., Tomilenko, A. A., Pokhilenko, N. P.
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Sprache:eng
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Zusammenfassung:This report presents the results of experimental studies of the fluid phase in the Fe-C-S system at high P and T values (5.3 GPa and 1300°C) conforming to diamond synthesis. The samples for experiments were mounted on air; therefore, the volatile compounds detected after the experiments are characterized by a wide variety and complicated composition involving both inorganic and organic components. Among the inorganic compounds, CO 2 , H 2 O, N 2 , SO 2 , CS 2 , and COS were detected. The GC/MS analysis revealed hydrocarbons (paraffins, olefins, and arenes), including high-molecular compounds. The formation of heavy hydrocarbons confirms their thermodynamic stability under high pressure. Oxygenated hydrocarbons (alcohols, aldehydes, ketones, carboxylic acids, and ethers) were also detected.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X15050219