2012
DOI: 10.1021/ic301677b
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Does Local Disorder Occur in the Pyrochlore Zirconates?

Abstract: The zirconates Ln(2)Zr(2)O(7) (Ln = lanthanoid) have been studied using a combination of Zr L-edge X-ray absorption near edge structure (XANES) and synchrotron X-ray and neutron powder diffraction methods. These studies demonstrate that as the size of the lanthanoid cation decreases, the local structure evolves smoothly from the ideal pyrochlore toward the defect fluorite rather than undergoing an abrupt transformation. The Zr L-edge spectrum is found to be extremely sensitive to changes in the local coordinat… Show more

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Cited by 104 publications
(118 citation statements)
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“…In both the lowest-energy A 2 B 2 O 7 -fluorite and weberite-type structures the average number of oxygen ions surrounding Zr (Ho) is 6.5 (7.5), compared to the number of 7 that would characterize a random distribution. This preference for lower (higher) coordination around the B 4+ (A 3+ ) cation is consistent with reverse Monte Carlo (RMC) analysis from neutron total scattering7 and X-ray absorption experiments2930 on zirconate and hafnate systems (i.e., A 2 B 2 O 7 , B=Zr, Hf), with a general trend towards increasing (decreasing) oxygen ion coordination of B (A) as the A cation size decreases (this trend is discussed in further detail in the next section). Similar coordination behavior was also found for titanate systems31; however, the local order was found to be pyrochlore, which is distinctly different compared to the preferred weberite-type configuration found here and in ref.…”
Section: Resultssupporting
confidence: 79%
“…In both the lowest-energy A 2 B 2 O 7 -fluorite and weberite-type structures the average number of oxygen ions surrounding Zr (Ho) is 6.5 (7.5), compared to the number of 7 that would characterize a random distribution. This preference for lower (higher) coordination around the B 4+ (A 3+ ) cation is consistent with reverse Monte Carlo (RMC) analysis from neutron total scattering7 and X-ray absorption experiments2930 on zirconate and hafnate systems (i.e., A 2 B 2 O 7 , B=Zr, Hf), with a general trend towards increasing (decreasing) oxygen ion coordination of B (A) as the A cation size decreases (this trend is discussed in further detail in the next section). Similar coordination behavior was also found for titanate systems31; however, the local order was found to be pyrochlore, which is distinctly different compared to the preferred weberite-type configuration found here and in ref.…”
Section: Resultssupporting
confidence: 79%
“…However, most of these pyrochlores are known to form disordered fluorite at high temperatures (see also Fig. 2 and the relevant text) and show experimental evidence for partial disordering [57], which is rather consistent with our result. The clear correlation of the smallness and negativeness of the AFP DFEs with the formation of the disordered fluorite strongly suggests that the easiness of defect formation on the oxygen sublattice is essential to the disordering of the pyrochlores and for subsequent formation of disordered fluorites.…”
supporting
confidence: 91%
“…Small deformations of the Bragg peaks have nevertheless been observed by means of diffuse neutron scattering experiments, which correspond to a local volume variation at the Pr site of about 1‰. These inhomogeneities, even small, could affect the magnetic properties, due to the sensitivity of non-Kramers doublets to local perturbations [4,[40][41][42]. Further studies are ongoing to investigate in details these inhomogeneities and their consequences.…”
Section: A Crystal Growthmentioning
confidence: 99%