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

The effects of (H(2)O)(n) (n = 1–3) clusters on the HO(2) + NH(2) → NH(3) + (3)O(2) 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, HO(2)⋯(H(2)O)(n) (n = 1–3) + NH(2) and H(2)N⋯(H(2)O)(n) (n = 1–3) + HO(2), are involved in the (H(2)O)(n) (n = 1–3) catalyzed HO(2) + NH(2) → NH(3) + (3)O(2) reaction. Due to the fact that HO(2)⋯(H(2)O)(n) (n = 1–3) complexes have much larger stabilization energies and much higher concentrations than the corresponding complexes of H(2)N⋯(H(2)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 H(2)O⋯HO(2) + NH(2) reaction being respectively larger by 5–6 and 6–7 orders of magnitude than the corresponding reactions of HO(2)⋯(H(2)O)(2) + NH(2) and HO(2)⋯(H(2)O)(3) + NH(2), the catalytic effect of (H(2)O)(n) (n = 1–3) is mainly taken from the contribution of the water monomer. In addition, the enhancement factor [Image: see text] 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.