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Tellus B: Chemical and Physical Meteorology
ISSN: (Print) 1600-0889 (Online) Journal homepage: www.tandfonline.com/journals/zelb20
15N/14N ratios of NO>x from vehicle engines and
coal-fired power stations
T. H. E. Heaton
To cite this article: T. H. E. Heaton (1990) 15N/14N ratios of NO>x from vehicle engines and coal-
fired power stations, Tellus B: Chemical and Physical Meteorology, 42:3, 304-307, DOI: 10.3402/
tellusb.v42i3.15223
To link to this article: https://doi.org/10.3402/tellusb.v42i3.15223
© 1990 The Author(s). Published by Taylor &
Francis.
Published online: 18 Jan 2017.
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Tel/us (1990), 42B, 304-307 
SHORT CONTRIBUTION 
15N/14N ratios of NOx from vehicle engines and coal-fired 
power stations 
By T. H. E. HEATON*, Natural Isotopes Division, NPRL, CS/R, P.O. Box 395, Pretoria, South Africa 
(Manuscript received 10 March 1989; in final form 13 June 1989) 
ABSTRACT 
Preliminary data are presented for the 15 N/ 14N ratios of the two main sources of 
anthropogenic NOx. Contrary to expectation, the b15 N values of NOx emitted from vehicle 
exhausts ( - 13 to - 2 %0 ) and coal-fired boilers ( + 6 to + 13 %0 ) are different from the isotopic 
composition of the nitrogen in their fuel+ air mixtures ( ~0%0). These differences may reflect 
variable effects of kinetic isotopic fractionation in the formation (vehicles) and destruction 
(boilers) of NO, and have important consequences for the use of nitrogen isotopes in 
atmospheric studies. 
1. Introduction 
Because nitrogen compounds play such an 
important role in the chemistry and pollution 
of the atmosphere, several studies have been 
directed towards an examination of their 
15N/ 14N ratios (Roering, 1957; Moore, 1977; 
Freyer, 1978; Heaton, 1986, 1987). The interpret­
ations of these studies, however, require infor­
mation on the isotopic composition of the NOx 
gases (NO and N02 ), for which very few data are 
available. 
The major sources for the anthropogenic 
emission of NOx are vehicles and coal-fired 
power stations. The nitrogen in their fuel + air 
combustion mixtures is either atmospheric N 2 (in 
vehicles) or atmospheric N 2 plus coal-nitrogen (in 
power stations). In both cases, this source 
nitrogen has a b15 N value which is equal to or 
close to 0 %0 : b 1 5 N = 0 %0 for atmospheric N 2 , 
b 1 5 N = typically - 2 to + 3 %0 for coals (see foot­
note to Table 1 for definition of b15N). It has 
therefore been assumed that the NOx gases 
formed by oxidation of this nitrogen will also 
*Present address: Isotope Geology Laboratory, 
Keyworth, Nottingham NG 12 5GG, England. 
have b15 N close to 0%0 (Freyer, 1978; Heaton, 
1987). Whilst a b15N value close to 0%0 for the 
anthropogenic emissions of NOx was partially 
supported by two earlier measurements of vehicle 
exhausts (b 15 N = -1.8 and +3.7%0 (Moore, 
1977; Freyer, 1978)), subsequent analyses of 
vehicle NOx suggested a wider range (b 15N = 
-13 to - 2 %0 , and a single analysis of NOx from 
a power station yielded b15N = +5%0 (Heaton, 
1987)). I therefore present 15N/14N ratio data for 
NOx from a further four vehicle exhausts and 
four power station emissions, and suggest 
possible mechanisms whereby the major sources 
of anthropogenic NOx may have b 15N values 
which are not close to 0%0 • The new data are 
discussed in conjunction with the earlier data 
presented, but not discussed, in Heaton (1987). 
2. Analytical method and precision 
Gases were sampled from the exhaust pipes of 
test-bed and road vehicle engines at Pretoria 
(altitude = 1300 m, no catalytic convertors) and 
from downstream of the electrostatic precipi­
tators of coal-fired boilers generating steam for 
electric power stations on the Transvaal Highveld 
Tellus 42B (1990), 3