A comprehensive examination of how the identity of an alcohol molecule can change the behavior of a solvated, alkaline earth dication has been undertaken. The metal dication of Ca
2+
has been clustered with a range of different alcohols to form [Ca(ROH)
n
]
2+
complexes, where
n
lies in the range 2–20. Following collisional activation via electron capture from nitrogen gas, complexes for
n
in the range 2–6 exhibit a switch in reaction product as a function of
n
. For low values, solvated CaOH
+
is the dominant fragment, but as
n
increases beyond 4, this is displaced by the appearance of solvated CaOR
+
. A separate study of unimolecular metastable decay by [Ca(ROH)
n
]
2+
complexes found evidence of charge separation to form CaOH
+
(ROH)
n
−1
+ R
+
. For two isomers of butanol, the
n
= 3 complexes were found to follow parallel, but different metastable pathways: one leading to the appearance of CaOH
+
and another that resulted in proton abstraction to form ROH
2
+
. These differences have been attributed to the precursor complexes adopting geometries where one ROH molecule occupies a secondary solvation shell. Comparisons were made with a previous study of magnesium complexes; [Mg(ROH)
n
]
2+
show that the difference in second ionization energy Mg
+
(15.09 eV) as opposed to Ca
+
(11.88 eV) influences behavior. A complex between Ca
2+
and 1-chloroethanol is shown to favor the formation of CaCl
+
as opposed to CaOH
+
as a unimolecular charge separation product, which is attributed to differences in bond energy in the precursor molecule.
Electronic supplementary material
The online version of this article (10.1007/s13361-019-02263-x) contains supplementary material, which is available to authorized users.