勃姆石
铝土矿
三水铝石
选区衍射
化学工程
材料科学
地质学
结晶学
镓
透射电子显微镜
矿物学
化学
纳米技术
冶金
工程类
铝
作者
Meng Liu,Wei Yin,Hao-Fan Jiang,Yuhan Wang,Qi-Tao Hu,Tian-Lei Zhao,Qi‐Zhi Yao,Sheng‐Quan Fu,Gen‐Tao Zhou
出处
期刊:American Mineralogist
[Mineralogical Society of America]
日期:2022-11-03
卷期号:108 (9): 1773-1780
被引量:1
摘要
Abstract Gallium (Ga) and aluminum (Al) belong to group IIIA elements in the periodic table. They show a coupled geochemical behavior in most natural systems and are considered as “geochemical partners.” However, compared with the principal oxyhydroxides of Al in nature, gibbsite [Al(OH)3], boehmite (γ-AlOOH), and diaspore (α-AlOOH), only the analogs söhngeite [Ga(OH)3] and tsumgallite (α-GaOOH) were reported. In this work, boehmite-type GaOOH (γ-GaOOH), a new polymorph of GaOOH, was synthesized for the first time using boehmite (γ-AlOOH) as a template. The synthesized γ-GaOOH was characterized by a series of techniques, including X-ray diffraction (XRD), high-angle annular dark-field scanning transmission electron microscopy (HAADF-STEM), and selected area electron diffraction (SAED). Furthermore, a model based on the boehmite structure was successfully applied to define the γ-GaOOH structure by the Rietveld method. Results from sample characterization and structural refinement support the successful synthesis of boehmite-type GaOOH, and thus it is referred to as γ-GaOOH. The synthesis of γ-GaOOH in the laboratory is valuable to understanding the Ga geochemistry and its enrichment process in Ga-rich boehmite in coal and bauxite.
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