天然锆石的局部结构、结构、振动和光学特性

Y. Kumar, Shilpa Tripathi, Pranesh Sengupta, S. N. Jha, Mangla Nand, Ayushi Trivedi, A. Sagdeo, Anupam Sharma, M. Tiwari, Vasant G Sathe, A. Arya
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引用次数: 0

摘要

通过将印度元锆石单晶体的结构特性与通过固态反应方法合成的合成锆石(作为标准)的结构特性进行比较,研究了印度元锆石单晶体的结构特性。X 射线衍射(XRD)数据揭示了晶格参数的变化以及应变、偏二甲化等现象的存在。研究发现,结晶度≈63.8%,表明同时存在结晶区和无序区。这些变化可能是由于多种放射性/非放射性元素的存在。通过全反射 X 射线荧光法观察了这些元素的存在并分析了样品成分。XRD 晶体学数据被进一步用作分析围绕 Zr 中心吸收原子记录的 X 射线吸收光谱数据的输入。与合成结构相比,X 射线吸收近缘结构显示出白线特征的轻微变化和一些无序。从扩展的 X 射线吸收精细结构中观察到的配位数减少表明局部结构中存在无序现象。显微拉曼光谱显示,不同位置的结晶行为各不相同,表明样品经历了不同程度的偏金属化,证实了元素的不均匀分布。这项工作记录并分析了与 Zr4+ 阳离子有关的孤立二氧化硅四面体网络的结构演变,它是数百万年来自我辐照和恢复的函数,并与光学特性相关联。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Local Structure, Structural, Vibrational, and Optical Properties of Natural Zircon
Structural properties of Indian metamict single zircon crystals are studied by comparing their properties with those of synthetic zircon synthesized via solid‐state reaction method, which serves as the standard. X‐Ray diffraction (XRD) data reveal changes in lattice parameters and the presence of strain, metamictization, etc. It is found that the degree of crystallinity is ≈63.8% indicating the simultaneous presence of crystalline and disordered regions. These changes are likely due to the presence of several radioactive/nonradioactive elements. The presence of such elements is observed and the sample composition is analyzed through total reflection X‐Ray fluorescence. XRD crystallographic data are further utilized as input for analyzing X‐Ray absorption spectroscopy data recorded around Zr central absorbing atom. X‐Ray absorption near‐edge structure shows slight modification in the white line feature and some disorder compared to the synthetic one. Reduced coordination number observed from extended X‐Ray absorption fine structure suggests the presence of disorder in local structure. Micro‐Raman spectroscopy indicates that crystalline behavior varies across different locations, suggesting that the sample has undergone varying degrees of metamictization, confirming a nonuniform distribution of elements. The work documents and analyses structural evolution within isolated silica tetrahedron network in association of Zr4+ cation as a function of self‐irradiation and recovery over millions of years and correlating the same with optical properties.
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