Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes...

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Theoretical Investigation of the M + RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner , Richard J. Plowright, Jack Graneek, Timothy G. Wright and W. H. Breckenridge 67 th International Symposium on Molecular Spectroscopy Ohio State University 22 nd June 2012

Transcript of Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes...

Page 1: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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

Page 2: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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).

Page 3: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

M+–RG Complexes: A Model of Solvation

Gardner et al., J. Phys. Chem. A., 114, 7631, (2010).

Page 4: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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).

Page 5: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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.

Page 6: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

0 60 120 180 240 300 360

-700

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He–Li+–He Bond Angle / oIn

tera

ction

Ene

rgy

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to th

e Li

+–He

+ H

e a

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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.

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“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.

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“Prototypical” Systems: Li+–Xe2

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Xe–Li+–Xe Bond Angle / oIn

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• 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.

Page 9: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

Open Shell Complexes: Be+–He2

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The calculated He-He bond length in the helium dimer is 3.06 Å.

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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.

Page 11: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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

Page 12: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

Open Shell Complexes: Be+–Ar2

Eint = -379 cm-1 Eint = +200 cm-1

Page 13: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

Open Shell Complexes: Be+–Ar2

Eint = -379 cm-1 Eint = +200 cm-1

Page 14: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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

Page 15: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

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+.

Page 16: Theoretical Investigation of the M + –RG 2 (M = Alkaline Earth Metal; RG = Rare Gas) Complexes Adrian M. Gardner, Richard J. Plowright, Jack Graneek, Timothy.

Prof. Timothy Wright Prof. Bill BreckenridgeDr. Richard PlowrightJack Graneek

Acknowledgements