In discussing ferrocene in the previous post, I mentioned Irving Langmuir’s 1921 postulate that filled valence shells in what he called complete molecules would have magic numbers of 2, 8, 18 or 32 electrons (deriving from the sum of terms in 2[1+3+5+7]). The first two dominate organic chemistry of course, whilst the third is illustrated by the transition series, ferrocene being an example of such. The fourth case is very much rarer, only one example ever having been suggested[1], it deriving from the actinides. In this post, I thought I would augment ferrocene (an 18-electron example) with beryllocene (an 8-electron example) and then speculate about 32-electron metallocenes.

Cp*-beryllocene. ELF analysis. Click for 3D.
Uranocene is a rather different beast. The ligands are not cyclopentadienyl, but cyclo-octatetraenyl. Uranium has a radon core, and a 5f3, 6d1 and 7s2 valence shell(s) electron configuration. Ionised to U4+, formally the 5f, 6d and 7p shells are all empty; a total of 14 + 10 + 6 electrons would be required to achieve a 32-electron filled shell , or 30 additional electrons. The two COT ligands, as di-anions (achieving aromaticity) could provide only 20. So uranocene (Cambridge refcode URACEN10, DOI 10.1021/ic50111a034) is far from the holy-grail of a 32-electron complete molecule.

Uranocene. AIM analysis. Click for 3D

Uranocene. ELF analysis. Click for 3D
References
- J. Dognon, C. Clavaguéra, and P. Pyykkö, "Towards a 32‐Electron Principle: Pu@Pb<sub>12</sub> and Related Systems", Angewandte Chemie International Edition, vol. 46, pp. 1427-1430, 2007. https://doi.org/10.1002/anie.200604198
- M.M. Conejo, R. Fernández, D. del Río, E. Carmona, A. Monge, and C. Ruiz, "Synthesis and structural characterization of Be(η<sup>5</sup>-C<sub>5</sub>Me<sub>5</sub>)(η<sup>1</sup>-C<sub>5</sub>Me<sub>4</sub>H). Evidence for ring-inversion leading to Be(η<sup>5</sup>-C<sub>5</sub>Me<sub>4</sub>H)(η<sup>1</sup>-C<sub>5</sub>Me<sub>5</sub>)", Chem. Commun., pp. 2916-2917, 2002. https://doi.org/10.1039/b208972f