Se. Rodriguez-cruz et al., Hydration energies and structures of alkaline earth metal ions, M2+(H2O)(n), n=5-7, M = Mg, Ca, Sr, and Ba, J AM CHEM S, 121(38), 1999, pp. 8898-8906
The evaporation of water from hydrated alkaline earth metal ions, produced
by electrospray ionization, was studied in a Fourier transform mass spectro
meter. Zero-pressure-limit dissociation rate constants for loss of a single
water molecule from the hydrated divalent metal ions, M2+(H2O)(n) (M = Mg,
Ca, and Sr for n = 5-7, and M = Ba for n = 4-7), are measured as a functio
n of temperature using blackbody infrared radiative dissociation. From thes
e values, zero-pressure-limit Arrhenius parameters are obtained. By modelin
g the dissociation kinetics using a master equation formalism, threshold di
ssociation energies (E-0,) are determined. These reactions should have a ne
gligible reverse activation barrier; therefore, E-0 values should be approx
imately equal to the binding energy or hydration enthalpy at 0 K. For the h
epta- and hexahydrated ions at low temperature, binding energies follow the
trend expected on the basis of ionic radii: Mg > Ca > Sr > Ba. For the hex
ahydrated ions at high temperature, binding energies follow the order Ca >
Mg > Sr > Ba. The same order is observed for the pentahydrated ions. Collis
ional dissociation experiments on the tetrahydrated species result in relat
ive dissociation rates that directly correlate with the size of the metals.
These results indicate the presence of two isomers for hexahydrated magnes
ium ions: a low-temperature isomer in which the six water molecules are loc
ated in the first solvation shell, and a high-temperature isomer with the m
ost likely structure corresponding to four water molecules in the inner she
ll and two water molecules in the second shell. These results also indicate
that the pentahydrated magnesium ions have a structure with four water mol
ecules in the first solvation shell and one in the outer shell. The dissoci
ation kinetics for the hexa- and pentahydrated clusters of Ca2+, Sr2+ and B
a2+ are consistent with structures in which all the water molecules ale loc
ated in the first solvation shell.