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Paramagnetic hole centres in natural zircon and zircon colouration

机译:顺磁性空穴以天然锆石和锆石着色为中心

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摘要

Paramagnetic defect centres and their relation to variable types of colouration were studied for eleven natural zircon crystals from three localities in North Carolina (USA), Massif Central (France), and Ural Mountains (Russia) using electron paramagnetic resonance (EPR) and optical absorption spectroscopy. The presence of tetragonal centres of trivalent rare-earth elements (REE3+) and niobium (Nb4+) irrespective of the colouration type and also in colourless grains suggests that these defects are not directly related to any specific zircon colouration. In contrast, the occurrence of two hole centres in crystals from North Carolina and the Massif Central correlates with the formation of specific broad bands in the absorption spectra. The appearance of pink colouration corresponds to the occurrence of a hole located at an oxygen nearest to Y3+ on zirconium site. This defect displays a single line at g = 2.006 in the EPR spectra for external magnetic field orientations parallel to the tetragonal crystal axis c. The related broad band in the optical absorption spectra peaks at 340-350 nm and its low-energy wing extends into the visible range. Reddish colour results from an intense broad absorption feature around 510-515 nm caused by a hole located at an oxygen next nearest to Y3+ substituting for Zr4+. A single line at g = 2.011 related to this "red" hole centre is observed in the EPR spectra in magnetic field orientation parallel c. The nature of the two paramagnetic centres was verified by their angular dependencies. Reddish-brownish and orange colour of zircon may appear for certain intensity relations between the two absorption bands with possible additional influence from charge transfer bands caused by Tb4+ centres. Yellowish-brownish colouration of zircon from the Ural Mountains is essentially different in nature. Several other paramagnetic defects with spin S = 1/2 were found in zircon from this locality besides the "red" hole centre, Tb4+, and REE3+ defects. There is a characteristic set of four bands in the optical absorption spectra. Additional heating and irradiation experiments are necessary for a correct assignment of paramagnetic defects to specific colour centres in this case.
机译:利用电子顺磁共振(EPR)和光学吸收光谱法研究了来自北卡罗来纳州(美国)、中央高原(法国)和乌拉尔山脉(俄罗斯)三个地区的11个天然锆石晶体的顺磁缺陷中心及其与不同颜色类型的关系。三价稀土元素 (REE3+) 和铌 (Nb4+) 的四方中心的存在,无论其着色类型如何,以及无色颗粒中的存在表明,这些缺陷与任何特定的锆石着色没有直接关系。相比之下,北卡罗来纳州和中央地块晶体中两个空穴中心的出现与吸收光谱中特定宽带的形成相关。粉红色的出现对应于位于锆位点上最接近 Y3+ 的氧处出现的孔。该缺陷在 EPR 光谱中显示一条 g = 2.006 处的单线,用于平行于四方晶轴 c 的外部磁场方向。光学吸收光谱中的相关宽带在340-350 nm处达到峰值,其低能翼延伸到可见光范围内。红色是由位于 Y3+ 取代 Zr4+ 的氧附近的氧处的孔引起的 510-515 nm 左右的强烈广泛吸收特征引起的。在平行 c 磁场方向的 EPR 光谱中观察到与该“红”洞中心相关的 g = 2.011 处的单线。两个顺磁性中心的性质通过它们的角度依赖性得到验证。锆石的红褐色和橙色可能出现在两个吸收带之间的某些强度关系中,并可能受到 Tb4+ 中心引起的电荷转移带的额外影响。来自乌拉尔山脉的锆石呈黄褐色,在性质上是不同的。除了“红”洞中心、Tb4+ 和 REE3+ 缺陷外,在这个地方的锆石中还发现了其他几个自旋 S = 1/2 的顺磁性缺陷。在光学吸收光谱中有一个由四个波段组成的特征集。在这种情况下,需要额外的加热和辐照实验才能将顺磁缺陷正确地分配给特定的颜色中心。

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