Experimental Binding Energies for the Metal Complexes [Mg(CH3OH)n]2+, [Ca(CH3OH)n]2+, and [Sr(CH3OH)n]2+ for n in the Range 4–20

Mg(II) and Ca(II) Microsolvation by Ammonia: Born-Oppenheimer Molecular Dynamics Studies

We report the structural and energetic features of the Mg²⁺ and Ca²⁺ cations in ammonia microsolvation environments. Born-Oppenhemier molecular dynamics studies are carried out for [Mg(NH₃)_n]²⁺ and [Ca(NH₃)_n]²⁺ clusters with n = 2, 3, 4, 6, 8, 20, and 27 at 300 K based on hybrid density functional theory calculations. We determine binding energies per ammonia molecule and the metal cation solvation patterns as a function of the number of molecules. The general trend for Mg²⁺ is that the Mg-N distances increase as a function of n until the first solvation shell is populated by six ammonia molecules, and then the distances slightly decrease while CN = 6 does not change. For Ca²⁺, the first solvation shell at room temperature is populated by eight ammonia molecules for clusters with more than one solvation shell, leading to a different structure from that of [Ca(NH₃)₆]²⁺ hexamine. The evaporation of NH₃ molecules was found at 300 K only for Mg²⁺ clusters with n ≥ 10; this was not the case for Ca²⁺ clusters. Vibrational spectra are obtained for all of the clusters, and the evolution of the main features is discussed. EXAFS spectra are also presented for the [Mg(NH₃)₂₇(NH₃)₂₇]²⁺ and [Ca(NH₃)₂₇]²⁺ clusters, which yield valuable data to be compared with experimental data in the liquid phase, as previously done for the aqueous solvation of these dications.

The Solvation of Ca2+ with Gas Phase Clusters of Alcohol Molecules

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 Ca²⁺ 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 ROH₂⁺. 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 Ca²⁺ 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.

Experimental measurements of water molecule binding energies for the second and third solvation shells of [Ca(H2O) n ]2+ complexes

Further understanding of the biological role of the Ca²⁺ ion in an aqueous environment requires quantitative measurements of both the short- and long-range interactions experienced by the ion in an aqueous medium. Here, we present experimental measurements of binding energies for water molecules occupying the second and, quite possibly, the third solvation shell surrounding a central Ca²⁺ ion in [Ca(H₂O) _n ]²⁺ complexes. Results for these large, previously inaccessible, complexes have come from the application of finite heat bath theory to kinetic energy measurements following unimolecular decay. Even at n = 20, the results show water molecules to be more strongly bound to Ca²⁺ than would be expected just from the presence of an extended network of hydrogen bonds. For n > 10, there is very good agreement between the experimental binding energies and recently published density functional theory calculations. Comparisons are made with similar data recorded for [Ca(NH₃) _n ]²⁺ and [Ca(CH₃OH) _n ]²⁺ complexes.

Experimental measurements of water molecule binding energies for the second and third solvation shells of [Ca(H2O) n ]2+ complexes

Further understanding of the biological role of the Ca²⁺ ion in an aqueous environment requires quantitative measurements of both the short- and long-range interactions experienced by the ion in an aqueous medium. Here, we present experimental measurements of binding energies for water molecules occupying the second and, quite possibly, the third solvation shell surrounding a central Ca²⁺ ion in [Ca(H₂O) _n ]²⁺ complexes. Results for these large, previously inaccessible, complexes have come from the application of finite heat bath theory to kinetic energy measurements following unimolecular decay. Even at n = 20, the results show water molecules to be more strongly bound to Ca²⁺ than would be expected just from the presence of an extended network of hydrogen bonds. For n > 10, there is very good agreement between the experimental binding energies and recently published density functional theory calculations. Comparisons are made with similar data recorded for [Ca(NH₃) _n ]²⁺ and [Ca(CH₃OH) _n ]²⁺ complexes.