【摘 要】
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A natural rutle sample was measured by in situ high-temperature X-ray diffraction (XRD) pattes, as well as Raman and Fourier transform infrared (FTIR). Crystal
【机 构】
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State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,
论文部分内容阅读
A natural rutle sample was measured by in situ high-temperature X-ray diffraction (XRD) pattes, as well as Raman and Fourier transform infrared (FTIR). Crystal structure is refined on the sample with 1.4 mol.% Fe and 510±120 ppmw. H2O. The unit-cell and TiO6 octahedral volumes are ex-panded by 0.7%–0.8% for Fe3+ incorporation, as compared with the reported Ti-pure samples. The volu-metric thermal expansion coefficient (α, K-1) could be approximated as a linear function of T (K): 4.95(3)× 10-9×T+21.54(5)×10-6, with the averaged value α0=30.48(5)×10-6 K-1, in the temperature range of 300–1500 K. The inteal Ti-O stretching (A1g and B2g) and O-Ti-O bending (Eg) modes show
ed shift, whereas the multi-phonon process exhibits lue shift at elevated temperature. The rotational mode (B1g) for TiO6 octahedra is nearly insensitive to temperature variations. The OH-stretching bands at 3279 and 3297 cm-1 are measured by high-temperature spectroscopy experiments. Both the IR-active and Raman-active OH-stretching modes shift to lower frequencies at higher temperature, with the signal intensities decreas-ing. And after quenching, we expect about 43% dehydration around 873 K, and 85% dehydration at 1273 K for this hydrous sample.
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