Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Migration of sulfur between organic and inorganic phases during hydrodesulfurization processes

Conference · · Preprints of Papers, American Chemical Society, Division of Fuel Chemistry; (USA)
OSTI ID:5436587

In the course of investigation of the non-isothermal hydrodesulfurization of model organic sulfur compounds in a coal-like environment with and without troilite, it was found that some of the non-thiophenic sulfur from the organic compounds was absorbed by troilite. This observation suggested that during hydrodesulfurization the organic sulfur had migrated to the inorganic phase. As the temperature was raised, more H{sub 2}S evolved from the sample with troilite, suggesting reevolution by pyrrhotite to trolite conversion. The purpose of this study was to use isotopic labeling to determine the mechanism of incorporation of sulfur into troilite. One possibility, as suggested by the formation of pyrrhotite confirmed by Moessbauer spectroscopy, that the H{sub 2}S produced from the organic compound was transferred to the inorganic phase, and then as the temperature was raised, H{sub 2}S evolution occurred from the troilite. Another possibility was that a direct reaction between the troilite and the organic compound took place, forming an intermediate followed by H{sub 2}S evolution from this intermediate as the temperature was raised. The fate and H{sub 2}S evolution profile from the labeling of the mobile organic sulfur group has been studied in an effort to distinguish possible mechanisms and demonstrate the role of troilite in this process.

OSTI ID:
5436587
Report Number(s):
CONF-8806313--
Journal Information:
Preprints of Papers, American Chemical Society, Division of Fuel Chemistry; (USA), Journal Name: Preprints of Papers, American Chemical Society, Division of Fuel Chemistry; (USA) Vol. 33:1; ISSN 0569-3772; ISSN ACFPA
Country of Publication:
United States
Language:
English