Structures of hydrated singly positive charged calcium−water clusters Ca+(H2O)n and their hydrogen-eliminated products (CaOH)+(H2O)n-1 were optimized using the ab initio molecular orbital methods and are compared with cationic magnesium−water clusters which have been investigated previously. For n ≥ 2, the structures of Ca+(H2O)n are different from those of Mg+(H2O)n. In the Mg+(H2O)n clusters, a pyramidical Mg+(H2O)3 forms the first shell. In contrast, a quasi-square-planar Ca+(H2O)4 is the first shell. The structures of (CaOH)+(H2O)n-1 are also different from structures (MgOH)+(H2O)n-1. The structural difference is attributed to the participation of the d orbitals of Ca atom in the bonding. Despite these structural differences, the core molecular ion (CaOH)+ in the hydrogen-eliminated products (CaOH)+(H2O)n-1 is very similar to the corresponding core ion (MgOH)+. Both ions, CaOH+ and MgOH+, are strongly polarized to Ca2+O-H and Mg2+O-H. Consequently, the hydration energies of the (CaOH)+(H2O)n are much larger than those of the corresponding Ca+(H2O)n. The internal energy change of the hydrogen-elimination reactions of the Ca+(H2O)n is positive for n = 1−4 but becomes negative for n ≥ 5, which is consistent with the product switch in the time-of-flight mass spectrum reported by Fuke's group. The equilibrium constants of the hydrogen elimination reaction are also consistent with the experimental observed isotope effects and the determined metal dependencies.
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