Multiple rare-earth ion environments in amorphous (Gd2O3)(0.230)(P2O5)(0.770) revealed by gadolinium K-edge anomalous x-ray scattering
Cole, Jacqueline M
Cramer, Alisha J
Shastri, Sarvjit D
Mukaddem, Karim T
Newport, Robert J
Physical Review Materials
American Physical Society
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Cole, J. M., Cramer, A. J., Shastri, S. D., Mukaddem, K. T., & Newport, R. J. (2018). Multiple rare-earth ion environments in amorphous (Gd2O3)(0.230)(P2O5)(0.770) revealed by gadolinium K-edge anomalous x-ray scattering. Physical Review Materials, 2 (045604) https://doi.org/10.1103/PhysRevMaterials.2.045604
A Gd K-edge anomalous x-ray scattering (AXS) study is performed on the rare-earth (R) phosphate glass, (Gd2O3)0.230(P2O5)0.770, in order to determine Gd⋯Gd separations in its local structure. The minimum rare-earth separation is of particular interest given that the optical properties of these glasses can quench when rare-earth ions become too close to each other. To this end, a weak Gd⋯Gd pairwise correlation is located at 4.2(1)Å, which is representative of a metaphosphate R⋯R separation. More intense first-neighbor Gd⋯Gd pairwise correlations are found at the larger radial distributions, 4.8(1), 5.1(1), and 5.4(1)Å. These reflect a mixed ultraphosphate and metaphosphate structural character, respectively. A second-neighbor Gd⋯Gd pairwise correlation lies at 6.6(1)Å which is indicative of metaphosphate structures. Meta- and ultraphosphate classifications are made by comparing the R⋯R separations against those of rare-earth phosphate crystal structures, R(PO3)3 and RP5O14, respectively, or difference pair-distribution function (ΔPDF) features determined on similar glasses using difference neutron-scattering methods. The local structure of this glass is therefore found to display multiple rare-earth ion environments, presumably because its composition lies between these two stoichiometric formulae. These Gd⋯Gd separations are well-resolved in ΔPDFs that represent the AXS signal. Indeed, the spatial resolution is so good that it also enables the identification of R⋯X(X=R, P, O) pairwise correlations up to r∼9Å; their average separations lie at r∼7.1(1), 7.6(1), 7.9(1), 8.4(1), and 8.7(1)Å. This is a report of a Gd K-edge AXS study on an amorphous material. Its demonstrated ability to characterize the local structure of a glass up to such a long range of r heralds exciting prospects for AXS studies on other ternary noncrystalline materials. However, the technical challenge of such an experiment should not be underestimated, as is highlighted in this work where probing AXS signal near the Gd K edge is found to produce inelastic x-ray scattering that precludes the normal AXS methods of data processing. Nonetheless, it is shown that AXS results are not only tractable but they also reveal local structure of rare-earth phosphate glasses that is important from a materials-centered perspective and which could not be obtained by other materials characterization methods.
J.M.C. is grateful to the Royal Commission of the Great Exhibition 1851 for a 2014 Design Fellowship hosted by Argonne National Laboratory (ANL) where work done was supported by the U.S. Department of Energy (DOE) Office of Science, Office of Basic Energy Sciences, and X-ray 1-BM beam line of the Advanced Photon Source, which is a DOE Office of Science User Facility, all under Contract No. DE-AC02-06CH11357. J.M.C. and R.J.N. are also indebted to the Engineering and Physical Sciences Research Council Grant No. GR/L41035 for funding.
External DOI: https://doi.org/10.1103/PhysRevMaterials.2.045604
This record's URL: https://www.repository.cam.ac.uk/handle/1810/278437
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