Jm. Martinez et al., STUDY OF THE AG-CHEMICAL SOLVATION MODEL( HYDRATION BY MEANS OF A SEMICONTINUUM QUANTUM), The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 101(24), 1997, pp. 4444-4448
The changes in the distance between the cation and the oxygen of the f
irst water shell (M-Or) induced by the rest of the solvent and the hyd
ration structure of Ag+ have been theoretically studied using a mixed
discrete-continuum model of solvation. Ab initio calculations at the M
P2 level for [Ag(H2O)(n)](+) clusters (n = 1, 2, 4, and 12, the last o
ne formed by two water shells (4 + 8)) in gas phase and solution were
carried out with DZ+polarization basis sets and Stevens et al.'s pseud
opotentials. The bulk solvent was simulated by means of Nancy's group
continuum solvation model. The clusters were placed in a cavity surrou
nded by a continuum with the static dielectric permittivity of the wat
er. Geometry optimization was performed in all cases. Calculations all
ow the examination of the specific interaction effects on the first so
lvation shell due to the hydrogen-bonded water molecules of the second
shell as well as the long-range interactions of the bulk solvent, des
cribed as a dielectric continuum. Likewise, the combination of both ef
fects is studied by the explicit consideration of a Ag+ polyhydrate co
ntaining two hydration shells, [Ag(H2O)(12)](+), immersed in a cavity.
Opposite effects on the Ag-Or distance were observed by the specific
and long-range (continuum) solvent interactions. Specific interactions
, mainly hydrogen bonding, shorten the bond, whereas long-range intera
ctions lengthen it, leading to a mutual partial cancellation of the ef
fects when the two types of interactions are jointly considered. Contr
ibutions to the Ag+ hydration enthalpy have also been examined in term
s of the semicontinuum model.