A novel method involving direct sampling of natural flame ions into a mass spectrometer has been used to measure the concentrations of HCN, NH3 and NO in atmospheric-pressure flames. It is found that HCN is formed from N~ in the reaction zone of rich hydrocarbon flames and is subsequently completely
The oxidation of hydrogen cyanide in fuel-rich flames
β Scribed by B.S. Haynes
- Publisher
- Elsevier Science
- Year
- 1977
- Tongue
- English
- Weight
- 557 KB
- Volume
- 28
- Category
- Article
- ISSN
- 0010-2180
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β¦ Synopsis
Over the temperature range 1950 to 2380 K, the rate constants k(12, ) --(2.0 -+ 0.2) X 108 m3/kgmolesec and k(is) = (5.6 +-0.7) Γ 1010 m3/kgmole-sec have been obtained. The relative contributions of reactions (12') and ( 15) vary markedly with'temperature, with reaction (15) dominating at temperatures above 2300 K. It is proposed that rupture of the OC-N linkage in the products of reactions (12') and ( 15) may then give rise to amine (N-H) species which are the measured products of HCN decay: +H HOCN --* HNCO --, NH 2 + CO, OCN+H ~ NH +CO. No evidence for any HCN-removing reactions involving CO2, NO or NH a has been obtained. while the appearance of HCN in unseeded flames may be due to reactions such as (3) [10] : CH + N 2 ~ HCN + N.
(3)
Given that HCN does occur in the appropriate post-flame gases, the purpose of this paper is to
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Green bands, attributed to HP0 by Lain Thanh My and Peyron, are emitted from the burnt gas o] [uel-rich flames containing a trace of trimethyl phosphate, but not [rom lean flames. Their intensity is proportional to [phosphorus]O.l+o.1 [HI 2 [H20~'~\_+Β°',~ [H,jJ o+\_,,.~ exp {--(5+5) kcal/RT} where [