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Theoretical Investigation of the M+–RG2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes
Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy G. Wright and W. H. Breckenridge
67th International Symposium on Molecular SpectroscopyOhio State University
22nd June 2012
M+–RG Complexes: A Model of Solvation• The M+–RG complexes are prototypical systems for the
investigation of solvation.
• Experimental studies have focused on the electronic spectroscopy of complexes containing alkaline earth metal cations.1
• The complexes of the closed shell alkali metal cations have been studied intensely using high level ab intio techniques.2
• Trends in equilibrium bond length and dissociation energy of the closed shell complexes are easy to rationalize.
• Whereas trends in the open shell M+–RG complexes were not!
1. See for example, M. A. Duncan, Annu. Rev. Phys. Chem., 48, 69, (1997).2. See for example, Breckenridge et al., Chem. Phys., 333, 77 (2007).
M+–RG Complexes: A Model of Solvation
Gardner et al., J. Phys. Chem. A., 114, 7631, (2010).
M+–RG Complexes: A Model of Solvation• The M+–RG complexes are prototypical systems for the
investigation of solvation.
• Experimental studies have focused on the electronic spectroscopy of complexes containing alkaline earth metal cations.1
• The complexes of the closed shell alkali metal cations have been studied intensely using high level ab intio techniques.2
• Trends in equilibrium bond length and dissociation energy of the closed shell complexes are easy to rationalize.
• Whereas trends in the open shell M+–RG complexes were not!
• In the present investigation aim to investigate increasing levels of solvation of Li+ and Be+ cations.
1. See for example, M. A. Duncan, Annu. Rev. Phys. Chem., 48, 69, (1997).2. See for example, Breckenridge et al., Chem. Phys., 333, 77 (2007).
Computational Methodology
• Standard aug-cc-pVTZ basis sets were employed for He, Ne and Ar.
• For Kr, and Xe the ECP10MDF and ECP28MDF effective core potentials along with the aug-cc-pwCVTZ-PP basis sets were utilized.
• For the metals, Li+ and Be+, aug-cc-pwCVTZ basis sets were employed.
• All calculations were carried out at the MP2 level of theory.
• Geometry optimizations and dissociation energies have been calculated using QZ and 5Z versions of the basis sets described above, but are not discussed herein.
• MOLPRO was used for all geometry optimization and energy calculations.
0 60 120 180 240 300 360
-700
-600
-500
-400
-300
-200
-100
0
He–Li+–He Bond Angle / oIn
tera
ction
Ene
rgy
Rela
tive
to th
e Li
+–He
+ H
e a
sym
ptot
e/ c
m-1
“Prototypical” Systems: Li+–He2
• A global minimum is found with a bond angle of 180o.
• The Li+–He bond length and dissociation energy calculated for the Li+–He2 complex is
almost identical to that of the Li+–He dimer complex.
• A stationary point is found with a linear Li+–He–He conformation, with the He–He separation shorter than calculated for the He2 cluster.
0 60 120 180 240 300 360
-640
-630
-620
-610
-600
-590
-580
He–Li+–He Bond Angle / oIn
tera
ction
Ene
rgy
/ cm
-1
“Prototypical” Systems: Li+–He2
• A very shallow minimum is observed at bond angle of ≈115o.
• This conformation has a slightly longer He–He bond length than in the He2 cluster.
“Prototypical” Systems: Li+–Xe2
0 60 120 180 240 300 360
-4000
-3500
-3000
-2500
-2000
-1500
-1000
-500
0
Xe–Li+–Xe Bond Angle / oIn
tera
ction
Ene
rgy
/ cm
-1
• A global minimum is found with a Xe–Li+–Xe bond angle of 180o.
• A second minimum is observed with a linear Li+–Xe–Xe conformation, with a Xe–Xe separation that is shorter than in the Xe2 cluster.
Open Shell Complexes: Be+–He2
0 60 120 180 240 300 360
-120
-100
-80
-60
-40
-20
0
He–Be+–He Bond Angle / oIn
tera
ction
Ene
rgy
/ cm
-1
The calculated He-He bond length in the helium dimer is 3.06 Å.
0 60 120 180 240 300 360
-2500
-2000
-1500
-1000
-500
0
Ar–Be+–Ar Bond Angle / oIn
tera
ction
Ene
rgy
/ cm
-1
Open Shell Complexes: Be+–Ar2
The calculated Ar-Ar bond length in the argon dimer is 3.77 Å
The De calculated for the Be+–Ar complex is 4050 cm-1.
Open Shell Complexes: Be+–Ar2
Δoccupancy Charge
Be+ +0.6892s -0.042px 0.022py 0.082pz 0.22Ar +0.1553s -0.033px -0.013py -0.063pz -0.05
Natural Population Analysis
Open Shell Complexes: Be+–Ar2
Eint = -379 cm-1 Eint = +200 cm-1
Open Shell Complexes: Be+–Ar2
Eint = -379 cm-1 Eint = +200 cm-1
Open Shell Complexes: Be+–Ar2
Eint = -379 cm-1 Eint = +200 cm-1
Δoccupancy Charge
Be+ +0.852s 0.002px 0.012py 0.012pz 0.12Ar +0.143s -0.023px -0.013py -0.013pz -0.10Ar +0.013s 0.003px 0.003py 0.003pz -0.01
Δoccupancy Charge
Be+ +0.852s 0.052px 0.012py 0.012pz 0.06Ar +0.073s -0.013px -0.013py -0.013pz -0.05Ar +0.073s -0.013px -0.013py -0.013pz -0.05
Δoccupancy Charge
Be+ +0.852s -0.022px 0.012py 0.012pz 0.13Ar +0.153s -0.023px -0.013py -0.013pz -0.10
Eint = -4050 cm-1
Conclusions
• Slices through the Li+–RG2 and Be+–RG2 potential energy surfaces have been presented and discussed.
• Even for the expectedly simple, closed shell Li+–RG2
complexes, multiple minima were observed.
• The linear RG–Li+–RG conformations were determined to be the most stable for all Li+–RG2 complexes.
• The Be+–RG2 surfaces were considerably more complicated.
• Bent RG–Be+–RG conformations were determined to be the most stable for all Be+–RG2 complexes.
• This was determined to be an effect of synergic interactions within the complex; sp2 hybridization of the Be+ orbital, and charge transfer from the RG2 dimer to Be+.
Prof. Timothy Wright Prof. Bill BreckenridgeDr. Richard PlowrightJack Graneek
Acknowledgements