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Kinetics and mechanisms of NOx - char reduction. Quarterly technical progress report, August 1, 1995--October 31, 1995
Author(s) -
Eric M. Suuberg,
W.D. Lilly,
I. Aarna
Publication year - 1996
Language(s) - English
Resource type - Reports
DOI - 10.2172/224293
Subject(s) - combustion , nox , char , context (archaeology) , coal , nitrogen oxides , chemistry , carbon fibers , coal combustion products , greenhouse gas , nitrogen , environmental science , environmental chemistry , waste management , organic chemistry , materials science , engineering , geology , paleontology , oceanography , composite number , composite material
The emission of nitrogen oxides from combustion of coal remains a problem of considerable interest, whether the concern is with acid rain, stratospheric ozone chemistry, or {open_quotes}greenhouse{close_quotes} gases. Whereas earlier the concern was focused mainly on NO (as a primary combustion product) and to a lesser extent NO{sub 2} (since it is mainly a secondary product of combustion), in recent years the emissions of N{sub 2}O have also captured considerable attention, particularly in the context of fluidized bed combustion, in which the problem appears to be most acute. The research community has only recently begun to take solid hold on the N{sub 2}O problem. This is in part because earlier estimates of the importance of N{sub 2}O in combustion processes were clouded by artifacts in sampling which have now been resolved. This project is concerned with the mechanism of reduction of both NO and N{sub 2}O by carbons. It was recognized some years ago that NO formed during fluidized bed coal combustion can be heterogeneously reduced in-situ by the carbonaceous solid intermediates of combustions. This has been recently supplemented by the knowledge that heterogeneous reaction with carbon can also play an important role in reducing emissions of N{sub 2}O, but that the NO-carbon reactions might also contribute to formation of N{sub 2}O. The precise role of carbon in N{sub 2}O reduction and formation has yet to be established, since in one case the authors of a recent study were compelled to comment that the basic knowledge of N{sub 2}O formation and reduction still has to be improved. The same can be said of the NO-carbon system

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