Kinetic study of the effect of sub-atmospheric conditions on the laminar burning velocity of high C2H6 content natural gas mixtures
The laminar burning velocity (S L ) was measured at sub-atmospheric pressure (0.84 atm) and an environmental temperature of 295 ± 2 K for two high C 2 H 6 content fuel mixtures, 75% CH 4 - 25% C 2 H 6 (mixture M1), and 50% CH 4 - 50% C 2 H 6 (mixture M2), as well as the pure constituent fuels. The e...
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Published in | Combustion theory and modelling Vol. 26; no. 2; pp. 338 - 364 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Taylor & Francis
23.02.2022
|
Subjects | |
Online Access | Get full text |
ISSN | 1364-7830 1741-3559 |
DOI | 10.1080/13647830.2021.2016981 |
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Summary: | The laminar burning velocity (S
L
) was measured at sub-atmospheric pressure (0.84 atm) and an environmental temperature of 295 ± 2 K for two high C
2
H
6
content fuel mixtures, 75% CH
4
- 25% C
2
H
6
(mixture M1), and 50% CH
4
- 50% C
2
H
6
(mixture M2), as well as the pure constituent fuels. The equivalence ratios for the experiments ranged between 0.8 and 1.4. Numerical calculations predicting S
L
were performed using 3 detailed reaction mechanisms, finding GRI-Mech 3.0 to achieve the best agreement at the pressure conditions evaluated. The pre-exponential factor of reaction H + O
2
= O + OH (R38) was modified in order to improve the numerical results at sub-atmospheric conditions. Kinetic analysis by means of the defined reaction factor (
) was carried out to identify the mechanism for S
L
changes at sub-atmospheric conditions. According to the experimental results, S
L
increased by 15.9% and 26.3% for mixtures M1 and M2, respectively, at 0.84 atm as compared to 1.0 atm. The reaction pathways elaborated employing F
R
indicate that the increase in S
L
at sub-atmospheric conditions is caused by increased CH
3
radical production by reaction C
2
H
5
+ H = 2CH
3
(R159), which increases the formation of H radical through reactions O + CH
3
= H + CH
2
O (R10) and O + CH
3
= H + H
2
+ CO (R284). The recombination reactions associated with the production of CH
4
and C
2
H
6
also contribute to S
L
increases at sub-atmospheric conditions. |
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ISSN: | 1364-7830 1741-3559 |
DOI: | 10.1080/13647830.2021.2016981 |