在质子间隔的WO4基中极地中心的结构 Scheelite-Type Tungstates
Georgijs Bakradze1, Edmund Welter2, Alexei Kuzmin1
1Institute of Solid State Physics, University of Latvia, 8 Kengaraga Street, LV-1063 Riga, Latvia.
Materials (Basel, Switzerland)
|July 13, 2024
概括
石灰的质子化引入了极子中心,通过将W6+减少到W5+,形成深蓝紫色. 这种结构变化涉及到[WO4]四面体内的H+间隙和W5+位移.
科学领域:
- 材料科学 材料科学 材料科学
- 固态化学 固态化学
- 频谱学是一种光谱学.
背景情况:
- 斯凯利特类化合物 (AWO4) 由于其多样化的特性而受到广泛研究.
- 了解缺陷中心及其对材料性能的影响对于开发新功能材料至关重要.
研究的目的:
- 为了研究在质子化石灰 (HWO4) 中极子中心的形成和结构特征.
- 阐明在质子化时W6+减少为W5+的机制.
主要方法:
- 射线吸收光谱 (W L3 边缘和 Sr K 边缘)
- 在X射线光电子光谱学 (XPS) 中.
- 反向蒙特卡洛 (RMC) 模拟
- 第一个原则计算计算.
主要成果:
- 通过酸电解质对AWO4 (A=Ca,Sr,Ba) 的质子化导致W5+极子中心的形成.
- XPS证实了W5+的存在,RMC分析显示这些中心周围的局部结构放松.
- 第一原理计算支持W5+离子从[WO4]四面体的中心移动.
结论:
- +的插入到石结构中驱动了W6+的减少到W5+,形成了极子中心.
- 这一过程导致了特有的深蓝紫色调和W5+离子周围的局部结构扭曲.
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