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New spectroscopic and diffraction data to solve the vanadium-doped zircon pigment conundrum

机译:新的光谱和衍射数据,解决钒掺杂锆石颜料难题

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摘要

The literature on V-doped zircon pigments offers a puzzling situation with unanswered questions about the origin of turquoise colour. In this study, new diffraction (XRPD) and spectroscopic (EPR, EAS) data were obtained on four industrial pigments, whose vanadium content is much higher than samples from previous investigations. Both EPR features and XRPD results indicate the occurrence of tetrahedrally-coordinated V4+at the zircon interstitial site 16g. EPR spectra at 5?K exhibit a structured multiplet attributed to isolated V4+ions and an exchange-narrowed line resulting by clustering of V4+ions. The intensity of optical bands is stronger in samples affected by V4+clusters. However, the turquoise colour stems from the window of transmitted green-bluish light, which depends on both the tail of the main optical band (2B???2A) and the onset of charge transfer phenomena. Small variations in these two bands readily turn into a chromatic shift from light blue to green.
机译:V-Doped锆石颜料的文献提供了一种令人费解的情况,具有关于绿松石颜色起源的难题问题。 在该研究中,在四种工业颜料上获得了新的衍射(XRPD)和光谱(EPR,EAS)数据,其钒含量远高于先前研究的样品。 EPR特征和XRPD结果都表明锆石间隙位点16G的四面体协调V4 +的发生。 在5Ω·k处的EPR光谱表现出归因于分离的V4 +离子的结构化多功能和通过聚集V4 +离子而产生的交换变窄线。 光带的强度在受V4 +簇影响的样本中更强。 然而,绿松石颜色源于透过的绿色蓝光窗口,这取决于主光学带(2b≤2a)的尾部和电荷转移现象的发作。 这两个条带中的小变化容易变成从浅蓝色到绿色的色转变。

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