U. Achatz et al., Hypoiodous acid as guest molecule in protonated water clusters: A combinedFT-ICR/DFT study of I(H2O)(n)(+), J AM CHEM S, 123(25), 2001, pp. 6151-6156
Cationic water clusters containing iodine, of the composition I(H2O)(n)(+),
n = 0-25, are generated in a laser vaporization source and investigated by
FT-ICR mass spectrometry. An investigation of blackbody radiation-induced
fragmentation of size-selected clusters I(H2O)(n)(+), n = 3-15, under colli
sion-free conditions revealed an overall linear increase of the unimolecula
r rate constant with cluster size, similar to what has been observed previo
usly for other hydrated ions. Above a certain critical size, I(H2O)(n)(+),
n greater than or similar to 13, reacts with HCl by formation of the interh
alide ICI and a protonated water cluster, which is the reverse of a known s
olution-phase reaction. Accompanying density functional calculations illust
rate the conceptual differences between cationic and anionic iodine-water c
lusters I(H2O)(n)(+/-). While I-(H2O)(n) is genuinely a hydrated iodide ion
, the cationic closed-shell species I(H2O)(n)(+) may be best viewed as a pr
otonated water cluster, in which one water molecule is replaced by hypoiodo
us acid. In the strongly acidic environment, HOI is protonated because of i
ts high proton affinity. However, similar to the well-known H3O+/H5O2+ cont
roversy in protonated water clusters, a smooth transition between H2IO+ and
H4IO2+ as core ions is observed for different cluster sizes.