Abstract
Graphite is being used as a carbon source for gasification to insure that hydrogen or hydrogen in hydrocarbons is derived from water. Relatively low temperatures (500–800K) are used to favor the equilibrium C+2H2O →CH4 +CO2 which is almost thermally neutral. In the presence of alkali hydroxide C2-C6 hydrocarbons are formed in addition to H2, CH4 and CO2. Formation of hydrocarbons is a stoichiometric reaction proceeding on the crystal edges to form a phenolate and hydrocarbons, e.g. 5C+4KOH 4COK+CH4. Surface spectroscopy has confirmed the presence of phenolate, which can be decomposed over metal oxide to make the reaction truly catalytic: \(44C0K\xrightarrow{{Me0x}}2{K_2}0 + 2C + 2C0\); 2K2O+2H2O→4KOH. In the presence of both KOH and metal oxide the major products are CO2 and H2 with traces of CH4 and CO. The 2:1 ratio of H2/CO2 appears due to either or both watergas shift and Boudouart reaction. The mechanisms will be illustrated by electron microscopy and XPS measurements.
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© 1986 D. Reidel Publishing Company, Dordrecht, Holland
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Heinemann, H., Somorjai, G.A. (1986). Mechanism of the Catalytic Gasification and Reactivity of Graphite. In: Setton, R. (eds) Chemical Reactions in Organic and Inorganic Constrained Systems. NATO ASI Series, vol 165. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-4582-1_29
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DOI: https://doi.org/10.1007/978-94-009-4582-1_29
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-8536-6
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