Abstract
Ab initio molecular orbital calculations on the higher hydrates of H3O+, using a split valence level basis set (4–31G), have led to the following results. (1) Energies for successive hydration are in good accord with gas‐phase thermochemical data. (2) Hydrogen‐bonded OH and O⋅⋅⋅O distances in H9O4+ are in excellent agreement with condensed phase diffraction data. (3) Large variations in OH (≲0.08 Å) and O⋅⋅⋅O (∼0.25 Å) distances caused by strong hydrogen bonding are monotonically correlated with OH stretching force constants and frequencies, which cover a range of 1500 cm−1. (4) Excellent quantitative correlation is obtained between calculated and observed infrared gas‐phase frequencies for six intense OH stretching bands, as represented by the least‐squares fit, νexp=−704+1440 (FSGS)1/2±15 cm−1. This least squares relationship is used to assign some of the other experimental absorption bands from the gas phase. The only major uncertainty is in the case of the symmetric H3O+ mode in H3O+(H2O)3. (5) The relative magnitudes of frequencies for symmetric (ν1) and antisymmetric (ν3) stretching modes are found to switch upon passing from H3O+13) to H3O+(H2O)31≳ν3). (6) The isoelectronic species H3O+(H2O)3 and OH(H2O)3 are predicted have very similar frequencies for symmetric stretching of hydrogen‐bonded OH groups, in accord with Raman data for aqueous acid. (7) Addition of a fourth water molecule to the first solvation shell of H3O+ does not lead to any significant stabilization, a result consistent with x‐ray and neutron diffraction results from aqueous HCl. (8) The most stable isomer of H13O6+ is found to be an H9O4+ moiety, somewhat perturbed from three‐fold symmetry by two second shell water molecules. (9) The tetrahydrate of the diaquahydrogen ion yields an H13O6+ structure 2.2 kcal/mole higher in energy and provides a possible model for the symmetric intermediate in aqueous proton transfer (observed activation energy, 2.4 kcal/mole). This model emphasizes the importance of concerted reorganization of OH and O⋅⋅⋅O bond lengths in the vicinity of the excess proton, with proton tunneling not expected to be a major factor, since the postulated intermediate offers a symmetric singlewell potential for the excess proton.

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