缅甸抹谷Baw-mar矿区蓝宝石的热处理及谱学研究
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昆明理工大学材料科学与工程学院

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P619.28

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国家自然科学(51662023)


Study on Heat Treatment and Spectroscopy of Sapphire from Baw-mar,Mogok,Burma
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China Faculty of Material Science and Engineer,Kunming University of Science And Technology,Yunnan

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    摘要:

    目前缅甸抹谷矿区开采的蓝宝石原石约80%都要经过优化处理才能投入市场,其中主要为热处理。本文对缅甸抹谷Baw-mar矿区蓝宝石进行不同温度制度的热处理,并利用X射线荧光光谱仪(XRF)、X射线粉晶衍射仪(XRD)、紫外-可见-近红外光谱仪(UV-VIS-NIR)、傅里叶红外光谱仪(FTIR)和激光拉曼光谱仪(Raman)对其热处理前后的光谱学特征进行对比研究。结果表明,1300℃热处理后所有2θ<60°的蓝宝石XRD衍射峰开始向低角度方向偏移,晶胞参数c/a比值随热处理温度升高而降低,表明其晶体结构在高温下发生畸变;Baw-mar矿区蓝宝石的主要致色元素是Fe、Ti和V,Ni是其产生灰色调的原因,热处理后样品中Fe2+-Ti4+离子对转移增强、Fe2+-Fe3+离子对转移减弱,导致紫外-可见-近红外光谱中588nm吸收带增强、746、764nm吸收峰减弱,同时样品颜色变蓝且灰色调减弱;红外光谱中,Baw-mar矿区蓝宝石存在1988、2123cm-1硬水铝石羟基倍频振动吸收峰和3619、3696cm-1高岭石外羟内羟振动吸收峰,热处理后由于硬水铝石和高岭石完全脱水,晶体结构被破坏导致羟基吸收峰全部消失;1100℃热处理后出现1324cm-1拉曼谱峰并随温度升高逐渐增强,推测其为高温下熔融硼砂和Al2O3反应形成玻璃态物质沿裂隙进入蓝宝石内部所致。本文通过光谱学特征分析为无损检测该矿区蓝宝石提供了可靠的鉴别数据,也为进一步探讨其改色工艺提供了思路和理论依据。

    Abstract:

    At present, about 80 percent of rough sapphire mined from the Mogok mine in Myanmar must be optimized before being put into the market, mainly heat treatment. In this paper, the sapphire from Baw-mar mine, Mogok, Myanmar is heat treated with different temperature regimes, and X-ray fluorescence spectrometer (XRF), X-ray powder crystal diffractometer (XRD), Ultraviolet-visible-near infrared spectrometer (UV-Vis-NIR), Fourier infrared spectrometer (FTIR) and Laser Raman spectrometer (Raman) were used to compare the spectroscopic characteristics before and after heat treatment. The results show that all sapphire XRD peaks with 2θ < 60° start to shift to low-angle after heat treatment at 1300℃, and the unit cell parameter c/a ratio decreases with the increase of heat treatment temperature, indicating that the crystal structure is distorted at high temperatures. The main color-causing elements of sapphire from Baw-mar mine are Fe, Ti, and V. Ni is the cause of the gray tone. After the heat treatment, the Fe2+-Ti4+ ion pair transfer is enhanced, and the Fe2+-Fe3+ ion pair transfer is weakened, resulting in an enhanced 585nm ultraviolet absorption band and a weakened absorption peak at 746 and 764nm. At the same time, the color of the sample turns blue and the gray tone weakens. In the infrared spectra, the sapphire from this mine has 1988, 2123cm-1 diaspore hydroxyl frequency doubled vibration absorption peaks and 3619, 3696cm-1 kaolinite outer hydroxyl and inner hydroxyl vibration absorption peaks. After the heat treatment, the diaspore and kaolinite are completely dehydrated, and the crystal structure is destroyed, resulting in the disappearance of all the hydroxyl absorption peaks. After heat treatment at 1100℃, the Raman peak at 1324cm-1 appeared and gradually increased with the increase of temperature. It is speculated that it is caused by the reaction of molten borax and Al2O3 at high temperature to form glassy substances along the cracks and enter the interior of the sapphire. This article provides reliable identification data for non-destructive testing of sapphire from this mine through spectroscopic feature analysis, and also provides ideas and theoretical basis for further discussion of its color modification process.

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  • 收稿日期:2021-05-21
  • 最后修改日期:2022-05-11
  • 录用日期:2022-06-04
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