“…In fact, at first, 30% of HO 2 in the atmosphere will form HO 2 Á Á ÁH 2 O with water vapor at 298 K; 27 this indicates that HO 2 Á Á ÁH 2 O is an important form; moreover, in previous studies on HO 2 + SO 2 , 28 HO 2 + SO 3 , 29 HO 2 + H 2 COO, 30 HO 2 + HO 2 , 17,31 HO 2 + O 3 , 32 HO 2 + NO 2 , 33 HO 2 + ClO, 34 and HO 2 + HClO 35 reactions, water molecules were found to play an important role in enhancing the stability of pre-reactive complexes and reducing the apparent activation energies of the transition states. In addition, the concentration of the formed H 2 OÁ Á ÁHO complex has been reported to be 5.5 Â 10 4 molecule cm À3 in the troposphere, 36 and previous studies on the water-catalyzed reactions HO + HOCl, 37 HCOOH + HO, 38 HO + H 2 O 2 , 39 HCHO + HO, 40 HO + HCl, 41 HO + CH 3 SO 3 H, 42 HO + CY 2 XH (X = H, F, OH, or NH 2 , and Y = H, CH 3 or F), 43 and HO + O 3 44 demonstrate how a single water molecule can catalyze a radical-molecule reaction involving HO radical; thus, the reactivity of HOÁ Á ÁH 2 O should also be taken into account. In these contexts, the important impact of water vapor on the atmospheric processes of the HO 2 + HO reaction may be not negligible.…”