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U.S. Department of Energy
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Importance of active sites for char gasification in oxygen (air) and carbon dioxide. Annual report, October 1984-September 1985

Technical Report ·
OSTI ID:5850425
Gasification reactivities, in air and carbon dioxide, were determined by isothermal and nonisothermal thermogravimetric methods for a range of coals and heat-treated coals. The coals were of varying rank, ranging from anthracite through lignite. Nonisothermal reactivity data, in air, clearly indicate that as coal rank increases there is a decrease in gasification reactivity. The measured reactivity of a heat-treated coal is strongly influenced by the rank of the parent coal, heat-treatment temperature, heat treatment conditions and the inorganic species present in the coke/char. The catalytic influence of inorganic species on reactivity is greatest for chars derived from low-rank coals (lignite and subbituminous). In some cases, significant reduction of the minerals in high-rank coals (low-volatile bituminous and anthracite) prior to carbonization can result in modest increases in reactivity. Oxygen chemisorption, under controlled conditions has been utilized to provide a measure of carbon active concentration in the chars/cokes.
Research Organization:
Pennsylvania State Univ., University Park (USA). Dept. of Materials Science and Engineering
OSTI ID:
5850425
Report Number(s):
PB-86-174463/XAB
Country of Publication:
United States
Language:
English