Fossil fuels such as coal and heavy fuel oils contain up to about 2 per cen
t by weight of fuel nitrogen, most of this being present in pyridine or pyr
olic aromatic structures. Under pyrolytic conditions these ring structures
decompose to give HCN and CH3CN. For present day computer modelling of NO,
formation in flames it is necessary to know the mechanism and rates of reac
tion. A number of previous studies of pyridine pyrolysis have been undertak
en using shock tubes or flow reactors. In this present study a shock tube w
as used to obtain the kinetics of pyridine decomposition in the range 1590-
2335 K and with pressures between 2.2 and 3.4 atm. Two independent sets of
data were obtained. One set of results was found to be represented by an Ar
rhenius rate constant k = 10(9.7+/-0.5) exp ( - 220.0 kJ mol(-1) RT-1)s(-1)
. For the other work k = 10(9.8+/-0.5) exp (-228.191 +/- 18.42 kJ mol(-1) R
T-1)s(-1).
In addition, the pyrolysis mixtures of pyridine plus toluene have also been
studied to understand the synergistic effects. The results indicated the s
trong involvement initiated by fission of the pyridine ring system. Copyrig
ht (C) 2000 John Wiley & Sons, Ltd.