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Structural stabilization of δ-phase Bi2O3 in the MgBi1.5RE0.5O4 system through rare earth substitution for improved ionic conductivity

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dc.contributor.author Renju, U A
dc.contributor.author Rao, P P
dc.date.accessioned 2021-10-27T06:23:42Z
dc.date.available 2021-10-27T06:23:42Z
dc.date.issued 2020-10
dc.identifier.citation Ionics;26(10):5113-5121 en_US
dc.identifier.uri https://doi.org/10.1007/s11581-020-03662-x
dc.identifier.uri http://hdl.handle.net/123456789/3826
dc.description.abstract Fluorite-structured Bi(2)O(3)oxide materials are promising candidates for oxygen ion conductors. In this regard, we attempted to stabilise the delta-phase through rare earth ion substitution in a new series of compositions: MgBi1.5RE0.5O4(RE = Nd, Sm, Gd, Dy, Y). They exhibit a phase transformation from a rhombohedral (Nd-Gd) to a fluorite-type (Dy, Y) structure as the ionic radius of rare earth decreases. The electrical property studies show that conductivity is a function of crystalline structure and lattice volume. Maximum conductivity of 4.3 x 10(-2) S/cm is obtained for the Y composition at 1023 K. The conductivity of the rhombohedral composition decreases as the lattice volume decreases associated with the increased activation energy. Contrastingly, the conductivity decreases with the increase of the lattice volume from Y to Dy on account of delta-phase instability at higher temperature. These results demonstrate that structural stabilization of delta-phase Bi(2)O(3)can be achieved through Y substitution with more thermal stability. en_US
dc.language.iso en en_US
dc.publisher Springer en_US
dc.subject delta-phase Bi2O3 en_US
dc.subject fluorite en_US
dc.subject conductivity en_US
dc.subject rare earth en_US
dc.title Structural stabilization of δ-phase Bi2O3 in the MgBi1.5RE0.5O4 system through rare earth substitution for improved ionic conductivity en_US
dc.type Article en_US


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    Research articles authored by NIIST researchers published in 2020

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