高级检索

    汪嘉伟, 王以群, 冯齐, 吴晓玉, 陈俊旭. 钴扩散越南蓝色尖晶石的紫外-可见-近红外光谱分析及鉴定[J]. 华东理工大学学报(自然科学版), 2018, 44(6): 839-844. DOI: 10.14135/j.cnki.1006-3080.20171218001
    引用本文: 汪嘉伟, 王以群, 冯齐, 吴晓玉, 陈俊旭. 钴扩散越南蓝色尖晶石的紫外-可见-近红外光谱分析及鉴定[J]. 华东理工大学学报(自然科学版), 2018, 44(6): 839-844. DOI: 10.14135/j.cnki.1006-3080.20171218001
    WANG Jia-wei, WANG Yi-qun, FENG Qi, WU Xiao-yu, CHEN Jun-xu. Analysis and Identification of Cobalt Lattice Diffused Vietnam Spinel by Using UV-Vis-NIR Spectroscopy[J]. Journal of East China University of Science and Technology, 2018, 44(6): 839-844. DOI: 10.14135/j.cnki.1006-3080.20171218001
    Citation: WANG Jia-wei, WANG Yi-qun, FENG Qi, WU Xiao-yu, CHEN Jun-xu. Analysis and Identification of Cobalt Lattice Diffused Vietnam Spinel by Using UV-Vis-NIR Spectroscopy[J]. Journal of East China University of Science and Technology, 2018, 44(6): 839-844. DOI: 10.14135/j.cnki.1006-3080.20171218001

    钴扩散越南蓝色尖晶石的紫外-可见-近红外光谱分析及鉴定

    Analysis and Identification of Cobalt Lattice Diffused Vietnam Spinel by Using UV-Vis-NIR Spectroscopy

    • 摘要: 选取越南产蓝色尖晶石样品进行成分测试,结果表明越南产尖晶石均是含微量Fe和Zn的镁铝尖晶石;经紫外-可见-近红外光谱测试,样品在230~800 nm范围内均有7个吸收带,且吸收带位置相对固定,说明Fe2+和Fe3+自旋禁阻跃迁及二者间的电荷耦合作用是蓝色尖晶石致色的主要原因;对比1 400℃下恒温24 h后Co扩散处理的样品,观察到460 nm附近及550~700 nm的宽吸收带更强,原因是Co离子进入尖晶石晶体,Co3+和Fe3+从八面体进入四面体后同相邻的Co2+和Fe2+共同作用,使得尖晶石色调变深,饱和度变高,经扫描电镜配合能谱仪测试后发现扩散深度约为10 μm。浸液法是检测扩散处理尖晶石较为有效的方法,经扩散处理的样品表面裂隙、凹坑处有颜色富集,放大后可见颜色分布不均匀,颜色艳丽、不自然。

       

      Abstract: The yield of blue spinel from Vietnam is high, while the spinel with excellent color and good quality is rare. Therefore, it is necessary to improve the color and the aesthetics for some blue spinel. Gray-blue spinel samples from the Luc Yen district Vietnam are selected for composition tests, according to the analysis of X-ray fluoresce (XRF) spectrum and laser-induced breakdown spectroscopy (LIBS). The spinel originated from Vietnam is magnesia-alumina spinel containing trace amount of Fe and Zn. By ultraviolet-visible-near infrared spectrum (UV-Vis-NIR), the samples have 7 absorption bands which approximately located at 371, 459, 478, 548, 580, 630, and 740 nm in the range of 230-800 nm. Besides, the positions of the absorption bands are relatively fixed, indicating that spin forbidden transitions between the Fe2+ and Fe3+ is the main reason for the color of natural blue spinel. The charge-coupled effect plays an important role in the color-change at the same time. Samples are compared before and after the cobalt lattice diffusion at the stable temperature of 1 400℃ for 24 h, and the treated samples are found to have stronger wide absorption bands located around 460 nm and 550-700 nm, because the cobalt ions pass into spinel's crystal structure. Co3+ and Fe3+ enter into the tetrahedron structure from the octahedron structure and then interact with adjacent Co2+ and Fe2+, which makes the color of the spinel's tone darker and the saturation more vivid. Through the analysis of scanning electron microscopy with energy dispersive spectrometer (SEM-EDS), the depth of diffusion is about 10 μm. The immersion method is effective for detecting the gray-blue spinel treated by lattice diffusion. The color district of samples after the lattice diffusion treatment gathers in surface crevice, and the color enriches in the pits too. Moreover, the color distribution is uneven and the color is unnatural.

       

    /

    返回文章
    返回