251. Catalytic effect of (H 2 O) n ( n = 1-3) on the HO 2 + NH 2 → NH 3 + 3 O 2 reaction under tropospheric conditions.
- Author
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Zhang T, Wang K, Qiao Z, Zhang Y, Geng L, Wang R, Wang Z, Zhao C, and Jin L
- Abstract
The effects of (H
2 O)n ( n = 1-3) clusters on the HO2 + NH2 → NH3 +3 O2 reaction have been investigated by employing high-level quantum chemical calculations with M06-2X and CCSD(T) theoretical methods, and canonical variational transition (CVT) state theory with small curvature tunneling (SCT) correction. The calculated results show that two kinds of reaction, HO2 ⋯(H2 O)n ( n = 1-3) + NH2 and H2 N⋯(H2 O)n ( n = 1-3) + HO2 , are involved in the (H2 O)n ( n = 1-3) catalyzed HO2 + NH2 → NH3 +3 O2 reaction. Due to the fact that HO2 ⋯(H2 O)n ( n = 1-3) complexes have much larger stabilization energies and much higher concentrations than the corresponding complexes of H2 N⋯(H2 O)n ( n = 1-3), the atmospheric relevance of the former reaction is more obvious with its effective rate constant of about 1-11 orders of magnitude faster than the corresponding latter reaction at 298 K. Meanwhile, due to the effective rate constant of the H2 O⋯HO2 + NH2 reaction being respectively larger by 5-6 and 6-7 orders of magnitude than the corresponding reactions of HO2 ⋯(H2 O)2 + NH2 and HO2 ⋯(H2 O)3 + NH2 , the catalytic effect of (H2 O)n ( n = 1-3) is mainly taken from the contribution of the water monomer. In addition, the enhancement factor of the water monomer is 10.06-13.30% within the temperature range of 275-320 K, which shows that at whole calculated temperatures, a positive water effect is obvious under atmospheric conditions., Competing Interests: The authors declare no conflicts of interest., (This journal is © The Royal Society of Chemistry.)- Published
- 2018
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