Computationally Accelerated Discovery of High Entropy Pyrochlore Oxides

Krishna Chaitanya Pitike, Antonio Macias, Markus Eisenbach, Craig A. Bridges, Valentino R. Cooper

Research output: Contribution to journalArticlepeer-review

22 Scopus citations

Abstract

High entropy ceramics provide enhanced flexibility for tailoring a wide range of physical properties, emerging from the diverse chemical and configurational degrees of freedom. Expanding upon the endeavors of recently synthesized high entropy ceramics in rock salt, fluorite, spinel, and perovskite structures, we explore the relative feasibility of formation of high entropy pyrochlore oxides, A2B2O7, with multication occupancy of the B-site, estimated from first-principles-based thermodynamic descriptors. Subsequently, we used Monte Carlo simulations to estimate the phase composition, oxygen vacancy concentration, and local ionic segregation as a function of temperature and oxygen partial pressure. In synergy with the theoretical calculations, we have investigated the synthesis of several multicomponent oxides with a pyrochlore composition, related to our computational investigations, resulting in four phase pure and one 97.4% pure high entropy pyrochlore oxides. Ultimately, our approach allows us to evaluate potential impurity phases, ionic disorder, and oxygen vacancy concentration in response to the experimental variables, thereby making realistic predictions that can direct and accelerate experimental synthesis of novel multicomponent ceramics.

Original languageEnglish
Pages (from-to)1459-1472
Number of pages14
JournalChemistry of Materials
Volume34
Issue number4
DOIs
StatePublished - Feb 22 2022

Funding

This manuscript has been authored by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the U.S. Department of Energy. The United States Government retains and the publisher, by accepting the article for publication, acknowledges that the United States Government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. The Department of Energy will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ). This work was supported by the U.S. Department of Energy (DOE), Office of Science, Basic Energy Sciences, Materials Sciences and Engineering Division. This research used resources of the Compute and Data Environment for Science (CADES) at the Oak Ridge National Laboratory (ORNL), which is supported by the Office of Science of the U.S. Department of Energy (DOE) under Contract No. DE-AC05-00OR22725, as well as the National Energy Research Scientific Computing Center (NERSC), which is supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC02-05CH11231. A.M. participated in this investigation by an appointment to the ORNL HERE Program, sponsored by the U.S. DOE and administered by the Oak Ridge Institute for Science and Education, while he was an undergraduate student at the University of California, Berkeley.

FundersFunder number
CADES
Data Environment for Science
U.S. Department of Energy
Office of Science
Basic Energy Sciences
Oak Ridge National LaboratoryDE-AC05-00OR22725, DE-AC02-05CH11231
Oak Ridge Institute for Science and Education
University of California Berkeley
Division of Materials Sciences and Engineering

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