“…Figure 2(a) shows the radial distribution functions (RDFs) for (BrO)Br· · ·O(water) and (BrO)O· · ·H(water). Interestingly, the results show that the RDF for (BrO)Br· · · O(water) exhibits a peak at the distance of r = 2.4 Å and a valley is at r = 2.8 Å, which is close to the (BrO)Br· · ·O(water) bond distance (2.8 Å) in the global-minimum configuration of the BrO·H 2 O complex at 0 K. 10,15,16 This result indicates that the interaction of (BrO)Br· · ·O(water) at the surface of a water slab is much weaker than that in the gas phase, due to the competitive interactions between (water)H· · ·O(water) and (BrO)Br· · ·O(water) in the water slab. On the other hand, the peak of the RDF for (BrO)O· · ·H(water) appears at r = 2.0 Å, consistent with the (BrO)O· · ·H(water) distance (2.0 Å) in the global-minimum configuration of the BrO·H 2 O complex at 0 K. 10,15,16 This result can be explained by the fact that water molecules tend to expose their H site at the air/water interface, which would favor the hydrogen bonding formation of (BrO)O· · ·H(water).…”