Ekaterina Kaneva, Olga Belozerova, Tatiana Radomskaya, Roman Shendrik
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引用次数: 0
摘要
研究了一种化学式为 (Fe3+ 0.74Zr0.64Ti0.46 Al0.15)(□1.02Na0.98)K[Li3Si12O30] 的环硅酸盐化合物--以铁为主的索格迭石。研究涉及对矿物样品的全面分析,包括晶体化学分析、拉曼光谱和傅立叶变换红外光谱、光学吸收和发光研究。通过单晶结构细化和电子探针显微分析确定了晶体学位点群。利用原位高温 X 射线衍射(30-750 °C)研究了粉末的热弹性行为。值得注意的是,没有检测到任何相变;索吉滇石表现出各向异性的热膨胀。研究人员首次研究了振动光谱和谱带分配。利用光学吸收和发光光谱研究了索格滇石中 d 5 离子杂质的电子跃迁。澄清了钠锰石粉红色和发光的起源。可见紫外光谱区的宽光谱带是索格淀石呈现粉红色的原因,这可能是由于 Fe3+ 离子中发生了 d-d 转变。
Crystal chemistry, Raman and FTIR spectroscopy, optical absorption, and luminescence study of Fe-dominant sogdianite
Fe-dominant sogdianite, a cyclosilicate compound with the chemical formula (Fe3+0.74Zr0.64Ti0.46 Al0.15)(□1.02Na0.98)K[Li3Si12O30], was studied. The investigation involved a comprehensive analysis of the mineral sample, including crystal-chemical analysis, Raman and FTIR spectroscopy, optical absorption, and luminescence study. Crystallographic site populations were determined through single crystal structure refinement and electron probe microanalysis. The thermoelastic behavior of a powder was studied using in situ high-temperature X-ray diffraction (30–750 °C). Notably, no phase transition was detected; sogdianite exhibited anisotropic thermal expansion. The first time study of vibrational spectra and spectral bands assigning were performed. The electronic transitions in d5-ion impurities of sogdianite were studied using optical absorption and luminescence spectroscopy. The origin of pink color and luminescence of sogdianite was clarified. The broad spectral bands in the visible UV spectral region are responsible for the pink color exhibited by sogdianite and could be attributed to d–d transitions occurring in Fe3+ ions.