The Role of Alkalis in Orchestrating Uranyl‐Peroxide Reactivity Leading to Direct Air Capture of Carbon Dioxide

Author:

Arteaga Ana12ORCID,Arino Trevor13ORCID,Moore Guy C.45,Bustos Jenna L.1,Horton Matthew K.45,Persson Kristin A.46ORCID,Li Jun1,Stickle William F.7,Kohlgruber Tsuyoshi A.2ORCID,Surbella Robert G.2ORCID,Nyman May1ORCID

Affiliation:

1. Department of Chemistry Oregon State University Corvallis OR, 97331 USA

2. Pacific Northwest National Laboratory 902 Battelle Blvd Richland WA 99354 USA

3. current address Department of Nuclear Chemistry U.C. Berkeley Berkeley California 94720 USA

4. Department of Materials Science and Engineering U. C. Berkeley California 94720 USA

5. Materials Science Division Lawrence Berkeley National Laboratory Berkeley CA 94720 USA

6. Molecular Foundry Lawrence Berkeley National Laboratory Berkeley CA 94720 USA

7. Hewlett-Packard, Inc 1040 NE Circle Blvd Corvallis OR 97330 USA

Abstract

AbstractSpectator ions have known and emerging roles in aqueous metal‐cation chemistry, respectively directing solubility, speciation, and reactivity. Here, we isolate and structurally characterize the last two metastable members of the alkali uranyl triperoxide series, the Rb+ and Cs+ salts (Cs‐U1 and Rb‐U1). We document their rapid solution polymerization via small‐angle X‐ray scattering, which is compared to the more stable Li+, Na+ and K+ analogues. To understand the role of the alkalis, we also quantify alkali‐hydroxide promoted peroxide deprotonation and decomposition, which generally exhibits increasing reactivity with increasing alkali size. Cs‐U1, the most unstable of the uranyl triperoxide monomers, undergoes ambient direct air capture of CO2 in the solid‐state, converting to Cs4[UVIO2(CO3)3], evidenced by single‐crystal X‐ray diffraction, transmission electron microscopy, and Raman spectroscopy. We have attempted to benchmark the evolution of Cs‐U1 to uranyl tricarbonate, which involves a transient, unstable hygroscopic solid that contains predominantly pentavalent uranium, quantified by X‐ray photoelectron spectroscopy. Powder X‐ray diffraction suggests this intermediate state contains a hydrous derivative of CsUVO3, where the parent phase has been computationally predicted, but not yet synthesized.

Funder

Basic Energy Sciences

Publisher

Wiley

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