Barluzzi, Luciano, Giblin, Sean R. ![]() ![]() |
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Abstract
The concept of oxidation state plays a fundamentally important role in defining the chemistry of the elements. In the f block of the periodic table, well-known oxidation states in compounds of the lanthanides include 0, +2, +3 and +4, and oxidation states for the actinides range from +7 to +2. Oxidation state +1 is conspicuous by its absence from the f-block elements. Here we show that the uranium(II) metallocene [U(η5-C5 i Pr5)2] and the uranium(III) metallocene [IU(η5-C5 i Pr5)2] can be reduced by potassium graphite in the presence of 2.2.2-cryptand to the uranium(I) metallocene [U(η5-C5 i Pr5)2]− (1) (C5 i Pr5 = pentaisopropylcyclopentadienyl) as the salt of [K(2.2.2-cryptand)]+. An X-ray crystallographic study revealed that 1 has a bent metallocene structure, and theoretical studies and magnetic measurements confirmed that the electronic ground state of uranium(I) adopts a 5f3(7s/6d z 2 )1(6d x 2–y 2 /6d xy )1 configuration. The metal–ligand bonding in 1 consists of contributions from uranium 5f, 6d, and 7s orbitals, with the 6d orbitals engaging in weak but non-negligible covalent interactions. Identification of the oxidation state +1 for uranium expands the range of isolable oxidation states for the f-block elements and potentially signposts a synthetic route to this elusive species for other actinides and the lanthanides.
Item Type: | Article |
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Date Type: | Published Online |
Status: | Published |
Schools: | Physics and Astronomy |
Additional Information: | License information from Publisher: LICENSE 1: URL: https://creativecommons.org/licenses/by/4.0/, Start Date: 2022-09-28 |
Publisher: | American Chemical Society |
ISSN: | 0002-7863 |
Date of First Compliant Deposit: | 14 October 2022 |
Date of Acceptance: | 23 September 2022 |
Last Modified: | 03 May 2023 22:11 |
URI: | https://orca.cardiff.ac.uk/id/eprint/153386 |
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