Are High-Temperature Molten Salts Reactive with Excess Electrons? Case of ZnCl2

Hung H. Nguyen, Vyacheslav S. Bryantsev, Claudio J. Margulis

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

Abstract

New and exciting frontiers for the generation of safe and renewable energy have brought attention to molten inorganic salts of fluorides and chlorides. This is because high-temperature molten salts can act both as coolants and liquid fuel in next-generation nuclear reactors. Whereas research from a few decades ago suggests that salts are mostly unreactive to radiation, recent experiments hint at the fact that electrons generated in such extreme environments can react with the melt and form new species including nanoparticles. Our study probes the fate of an excess electron in molten ZnCl2 using first-principles molecular dynamics calculations. We find that on the time scale accessible to our study, an excess electron can be found in one of three states; the lowest-energy state can be characterized as a covalent Zn2Cl5•2- radical ion, the other two states are a solvated Zn•+ species (ZnCl3•2-) and a more delocalized species that still has some ZnCl3•2- character. Since for each of these, the singly occupied molecular orbital (SOMO) where the excess charge resides has a distinct and well-separated energy, the different species can in principle be characterized by their own electronic spectra. The study also sheds light onto what is commonly understood as the spectrum of a transient radical species which can be from the SOMO onto higher energy states or from the melt to pair with the excess electron leaving a hole in the liquid.

Original languageEnglish
Pages (from-to)9155-9164
Number of pages10
JournalJournal of Physical Chemistry B
Volume127
Issue number42
DOIs
StatePublished - Oct 26 2023

Funding

This work was supported as part of the Molten Salts in Extreme Environments (MSEE) Energy Frontier Research Center, funded by the U.S. Department of Energy Office of Science, Office of Basic Energy Sciences. MSEE work at the University of Iowa was supported under a subcontract from Brookhaven National Laboratory, which is operated under DOE contract DE-SC0012704. Work at ORNL was supported by DOE contract DE-AC05-00OR22725. This research used resources of the Compute and Data Environment for Science (CADES) at the Oak Ridge National Laboratory and the National Energy Research Scientific Computing Center (NERSC), which are supported by the Office of Science of the U.S. Department of Energy under contracts nos. DE-AC05-00OR22725 and DE-AC02-05CH11231, respectively. H.H.N. and C.J.M. acknowledge the University of Iowa High Performance Computing Facility.

FundersFunder number
CADES
Data Environment for Science
University of Iowa High Performance Computing Facility
U.S. Department of EnergyDE-AC05-00OR22725, DE-AC02-05CH11231, DE-SC0012704
Office of Science
Basic Energy Sciences
Oak Ridge National Laboratory
Brookhaven National Laboratory

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