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) × 1010 m3/kgmole-sec have been obtained. The relative contributions of reactions (12') and ( 15) vary markedly with'temperature, with reaction (15) dominating at temperatur
Phosphorus in the burnt gas from fuel-rich hydrogenoxygen flames
✍ Scribed by C.P. Fenimore; G.W. Jones
- Publisher
- Elsevier Science
- Year
- 1964
- Tongue
- English
- Weight
- 324 KB
- Volume
- 8
- Category
- Article
- ISSN
- 0010-2180
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✦ Synopsis
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~'~_+°',~ [H,jJ o+_,,.~ exp {--(5+5) kcal/RT} where [phosphorus] represents the addition of trimethyl phosphate. The dependence on [H]2 is good to the nearest integral power. The uncertainty by the [actor {[H=,O]/CH ]} °'s reflects the small change in this quantity in most o[ the experiments. An interpretation is Offered which is consistent with the identification o[ the emitter as HPO: that the flame intensity is proportional to [H] [PO], and that the phosphorus is present mostly as P=, molecules which are equilibrated according to: P2+O :P +PO P +OH~PO+H
The flame result can also be interpreted by an intensity proportional to [H] [P~ with the same equilibria among P'2" PO and P. On either interpretation, the phosphorus must be considered to be mainly present as P2 molecules.
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