This paper is dedicated to Professor Siger~c Huzitzcrga or1 the occasiorz of his 65th birthdayMARIUSZ KLOBUKOWSKI. Can. J. Chem. 70, 589 (1992).SCF and Moiler-Plesset calculations were done for the hydrated alkaline-earth ions in the gas phase. The systems studied were M2+(H20),,, where M = Mg, Ca, and Sr, and rz = 1, 2, 3, 4 , and 6. The successive ion-water bond energies were in the range anticipated on the basis of extrapolation of results from experimental studies on larger hydrates. Introduction Recently, an experimental breakthrough achieved by Kebarle and co-workers (1) allowed for experimental studies in the gas phase of the equilibria involving water molecules and bivalent ions of the alkaline-earth elements: