The proton and water affinities of the Li + cation are predicted from ab initio molecular orbital theory using Gaussian 90 and Gaussian 92. These calculations were undertaken in order to understand the role that the hydrated Li + cation has in controlling acidity within the clay interlayers. Proton affinities for hydrated Li-(OH) complexes increase with increasing degree of hydration but level off above two waters. This results in the highest acidity for the Li + complex with fewer than two waters of hydration. Acidity is controlled by the effective charge on the Li + cation. Stabilization of the charge by associated water molecules contributes to the reduced acidity at higher hydration numbers. Implication of a tight, inner sphere coordination complex is suggested from the calculations. The calculations imply that acidity in Li + clays is relatively independent of the degree of hydration. Comparison with experimentally-derived hydration data for smectite clays reveals that sufficient water exists within the clay layers even at low relative humidities to fully hydrate the Li + cation. The calculated proton affinities for Li(OH)(H 2 O) n (298 K) are 238, 252, 251, and 253 kcal/mol for n ) 0, 1, 2, and 3, respectively. The calculated water affinities (tendency for a cation to adsorb water for Li(H 2 O) n + (298 K) are 29.5, 16.5, 7.0, and 9.5 kcal/mol for n ) 1, 2, 3, and 4, respectively. The water affinities obey the same trends as both experimentally determined water affinities and those of a recent theoretical paper but are consistently lower in value.