When Core Orbitals Act as Valence Orbitals: Linear and Bent Geometries of <i>MX</i> <sub>2</sub> for <i>X</i> a Halogen and <i>M</i> an Alkaline Earth

Although the VSEPR model predicts the group 2 dihalides to be linear, it has long been known experimentally that the dihalides of the heavier group 2 metals are bent. High-level <i>ab initio</i> CCSD(T)/awQ(-PP) and CASPT2/awQ(-PP) calculations were performed for the ground states of MX<sub>2</sub> (<i>M</i> = Be, Mg, Ca, Sr, Ba, and Ra; <i>X</i> = F, Cl, Br, and I) to predict optimized geometries, inversion barriers, bending frequencies, and natural orbitals. The MF<sub>2</sub> for <i>M</i> = Be and Mg; the MCl<sub>2</sub> for <i>M</i> = Be, Mg, and Ca; the MBr<sub>2</sub> for M = Be, Mg, Ca, and Sr; and the MI<sub>2</sub> for <i>M</i> = Be, Mg, Ca, and Sr are predicted to be linear. SrCl<sub>2</sub> is linear at the CASPT2 level but is slightly bent (quasilinear) at the CCSD(T) level. Inversion barriers to linearity increase down the column for a given halogen. The bending harmonic frequencies of CaF<sub>2</sub> and SrCl<sub>2</sub> are comparable to the inversion barriers, so the molecules are predicted to be quasilinear at most temperatures and highly fluxional. Natural orbitals at the SA-CASSCF level show a mixing of the outer core p<sub>n-1</sub> orbitals of the alkaline earth with the valence s and p orbitals of the halides for MF<sub>2</sub> (<i>M</i> = Ca, Sr, Ba, and Ra), MCl<sub>2</sub> (<i>M</i> = Sr, Ba, and Ra), MBr<sub>2</sub> (<i>M</i> = Ba and Ra), and MI<sub>2</sub> (<i>M</i> = Ba and Ra), which drives the bending. BaF<sub>2</sub> and RaF<sub>2</sub> also exhibit mixing of the outer core s<sub><i>n</i>-1</sub> orbitals with the 2s orbitals of F, which makes the bending more pronounced and the inversion barriers larger for these two molecules. All-electron calculations and population analysis suggest that the core d and valence d orbitals have only a small contribution to the bending. Ionicity increases down the column and decreases from the difluorides to the diiodides. Bending in these dihalides can be simply explained in terms of the outer core orbitals of the alkaline earth mixing with the valence of the halogens as they overlap the valence energy space of the halogens. Thus, the VSEPR model for predicting the bond angle for the Group 2 dihalides is good to on the order of ± 5 kcal/mol.

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Journal
Journal of the American Chemical Society
Published
2025-12-22
DOI
https://doi.org/10.1021/jacs.5c16443
Citations
1
Primary Topic
Inorganic Fluorides and Related Compounds
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article
Field-Weighted Citation Impact
0.54
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article

When Core Orbitals Act as Valence Orbitals: Linear and Bent Geometries of MX 2 for X a Halogen and M an Alkaline Earth

David A. Dixon, João Gabriel Farias Romeu
1 citations
Journal of the American Chemical Society
Inorganic Fluorides and Related Compounds
0.54
article

When Core Orbitals Act as Valence Orbitals: Linear and Bent Geometries of MX 2 for X a Halogen and M an Alkaline Earth

David A. Dixon, João Gabriel Farias Romeu
article en
1 citations

Abstract

Although the VSEPR model predicts the group 2 dihalides to be linear, it has long been known experimentally that the dihalides of the heavier group 2 metals are bent. High-level <i>ab initio</i> CCSD(T)/awQ(-PP) and CASPT2/awQ(-PP) calculations were performed for the ground states of MX<sub>2</sub> (<i>M</i> = Be, Mg, Ca, Sr, Ba, and Ra; <i>X</i> = F, Cl, Br, and I) to predict optimized geometries, inversion barriers, bending frequencies, and natural orbitals. The MF<sub>2</sub> for <i>M</i> = Be and Mg; the MCl<sub>2</sub> for <i>M</i> = Be, Mg, and Ca; the MBr<sub>2</sub> for M = Be, Mg, Ca, and Sr; and the MI<sub>2</sub> for <i>M</i> = Be, Mg, Ca, and Sr are predicted to be linear. SrCl<sub>2</sub> is linear at the CASPT2 level but is slightly bent (quasilinear) at the CCSD(T) level. Inversion barriers to linearity increase down the column for a given halogen. The bending harmonic frequencies of CaF<sub>2</sub> and SrCl<sub>2</sub> are comparable to the inversion barriers, so the molecules are predicted to be quasilinear at most temperatures and highly fluxional. Natural orbitals at the SA-CASSCF level show a mixing of the outer core p<sub>n-1</sub> orbitals of the alkaline earth with the valence s and p orbitals of the halides for MF<sub>2</sub> (<i>M</i> = Ca, Sr, Ba, and Ra), MCl<sub>2</sub> (<i>M</i> = Sr, Ba, and Ra), MBr<sub>2</sub> (<i>M</i> = Ba and Ra), and MI<sub>2</sub> (<i>M</i> = Ba and Ra), which drives the bending. BaF<sub>2</sub> and RaF<sub>2</sub> also exhibit mixing of the outer core s<sub><i>n</i>-1</sub> orbitals with the 2s orbitals of F, which makes the bending more pronounced and the inversion barriers larger for these two molecules. All-electron calculations and population analysis suggest that the core d and valence d orbitals have only a small contribution to the bending. Ionicity increases down the column and decreases from the difluorides to the diiodides. Bending in these dihalides can be simply explained in terms of the outer core orbitals of the alkaline earth mixing with the valence of the halogens as they overlap the valence energy space of the halogens. Thus, the VSEPR model for predicting the bond angle for the Group 2 dihalides is good to on the order of ± 5 kcal/mol.

Journal of the American Chemical SocietyVol. 148(1)
University of Alabama (US)
Openalex Percentile: Top 27%
Inorganic Fluorides and Related Compounds
0.54
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