Fast ion conductivity in strained defect-fluorite structure created by ion tracks in Gd2Ti2O7

Dilpuneet S. Aidhy, Ritesh Sachan, Eva Zarkadoula, Olli Pakarinen, Matthew F. Chisholm, Yanwen Zhang, William J. Weber

Research output: Contribution to journalArticlepeer-review

37 Scopus citations

Abstract

The structure and ion-conducting properties of the defect-fluorite ring structure formed around amorphous ion-tracks by swift heavy ion irradiation of Gd2Ti2O7 pyrochlore are investigated. High angle annular dark field imaging complemented with ion-track molecular dynamics simulations show that the atoms in the ring structure are disordered, and have relatively larger cation-cation interspacing than in the bulk pyrochlore, illustrating the presence of tensile strain in the ring region. Density functional theory calculations show that the non-equilibrium defect-fluorite structure can be stabilized by tensile strain. The pyrochlore to defect-fluorite structure transformation in the ring region is predicted to be induced by recrystallization during a melt-quench process and stabilized by tensile strain. Static pair-potential calculations show that planar tensile strain lowers oxygen vacancy migration barriers in pyrochlores, in agreement with recent studies on fluorite and perovskite materials. In view of these results, it is suggested that strain engineering could be simultaneously used to stabilize the defect-fluorite structure and gain control over its high ion-conducting properties.

Original languageEnglish
Article number16297
JournalScientific Reports
Volume5
DOIs
StatePublished - Nov 10 2015

Funding

This research was supported by the US Department of Energy, Office of Science, Basic Energy Sciences, Materials Science and Engineering Division. This research used resources of the National Energy Research Scientific Computing Center, supported by the Office of Science, US Department of Energy under Contract No. DEAC02-05CH11231 for the DFT calculations and MD simulations of ion track formation. The MD simulations of oxygen diffusivity were carried out using the Cascade computer cluster at EMSL, a national scientific used facility sponsored by USDOE, located at PNNL.

FundersFunder number
Materials Science and Engineering Division
US Department of Energy
Office of Science
Basic Energy Sciences

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