scholarly journals Supplementary material to "On the similarities and differences between the products of oxidation of hydrocarbons under simulated atmospheric conditions and cool-flames"

Author(s):  
Roland Benoit ◽  
Nesrine Belhadj ◽  
Maxence Lailliau ◽  
Philippe Dagaut
1969 ◽  
Vol 73 (10) ◽  
pp. 3395-3406 ◽  
Author(s):  
Ching-Huan Yang ◽  
Brian F. Gray

Studies have been made of the spontaneous ignition of n -heptane+oxygen+inert gas mixtures at temperatures from 440 to 650°C, where ignition takes place by a one-stage process and no cool flames are observed. Detailed measurements have been made of the variation of minimum ignition pressure with such factors as the temperature, the composition of the mixture undergoing ignition and the nature, shape and extent of the surface of the reaction vessel. In particular, experiments in a wide variety of vessels show that the surface parameter which primarily determines the ignition tendency is the average distance of the molecules from the walls, rather than the surface:volume ratio. The quantitative relations observed experimentally are compared with the predictions of two isothermal chain-branching mechanisms involving distinct chemical paths and with the consequences of the theory of thermal ignition. It is shown that the results in small vessels (volume < 500 cm 3 ) are best explained in terms of an isothermal chain mechanism involving hydrogen peroxide as degenerate-branching agent, although in larger vessels thermal factors probably become increasingly important.


A detailed analytical study of the cool-flame oxidation of propane has been carried out using a continuous-flow technique with a view to the further elucidation of the mechanism of the low-temperature oxidation of hydrocarbons. The formation of the three theoretically possible aldehydes has been demonstrated and the initially formed peroxide shown to be hydrogen peroxide. Measurements of the yields of the different products formed under varying conditions of temperature, composition and time of contact have been made and correlated with measurements of the luminous intensity and temperature of the flame. The results confirm the earlier conclusions of Norrish (1948) that aldehydes are the important branching agents in the temperature range of 300 to 400°C, and a detailed scheme based on that proposed earlier has been developed to account for the observations. The scheme has further been shown to allow of a simple explanation of the origin of the periodic character of the cool flame in terms of the thermal instability of the normal slow reaction.


2020 ◽  
Author(s):  
Roland Benoit ◽  
Nesrine Belhadj ◽  
Maxence Lailliau ◽  
Philippe Dagaut

Abstract. Whereas the kinetics of oxidation of limonene has been extensively studied and mechanisms for its oxidation by OH and/or ozone have been proposed, more studies are required for better understanding its oxidation pathways. The oxidation of limonene-oxygen-nitrogen mixtures was studied using a jet-stirred reactor at elevated temperature and atmospheric pressure. Samples of the reacting mixtures were collected and analyzed by high resolution mass spectrometry (Orbitrap) after direct injection or after separation by reverse-phase ultra-high-pressure liquid chromatography and soft ionization by (+/−) HESI and (+/−) APCI. The results indicate that among the 1138 detected products, many oxygenates found in earlier studies of limonene oxidation by OH and/or ozone are also produced under the present conditions. Other highly oxygenated products and oligomers were also detected in the present work. The results are discussed in terms of reaction pathways involving the initial formation of peroxy radicals, isomerization reactions yielding keto-hydroperoxides and other oxygenated intermediates and products up to C25H32O17. The possible occurrence of the Waddington mechanism and of the Korcek mechanism are also discussed. The present work demonstrates similarities between the oxidation products and oxidation pathways of limonene under simulated atmospheric conditions and in those encountered during the self-ignition of hydrocarbons at low temperatures, which should stimulate future interactions between communities of atmospheric chemistry and combustion chemistry to improve current chemical models.


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