赞比亚锰铝榴石的宝石学和化学成分特征

Gemmological and Chemical Characteristics of Spessartine from Zambia

  • 摘要: 赞比亚Lundazi地区是锰铝榴石的较新产地,对该产地一批橙黄色石榴石样品的化学成分、宝石学与光谱学特征进行了系统研究,提取出有意义的宝石学数据,丰富了该产地溯源信息。通过常规宝石学测试和化学成分测试,确定了赞比亚橙黄色石榴石为端元组分含量高至92 mol.%的锰铝榴石; 拉曼光谱与红外光谱的测试结果表明赞比亚锰铝榴石的3个特征拉曼峰分别位于907、551、349 cm-1附近,特征红外光谱分别位于976、891、865、629、571、522 cm-1附近; 通过分析赞比亚锰铝榴石的紫外-可见吸收光谱与谱峰归属,发现赞比亚锰铝榴石的橙黄色由Mn2+和Fe2+所致,对应的吸收峰分别为409、421、430、460、482nm和504、525、570nm。

     

    Abstract: The Lundazi region of Zambia is a relatively new source of spessartine. In this paper, a batch of orange-yellow garnet samples from this area were systematically studied in terms of chemical compositions and gemmological and spectral characteristics. Meaningful gemmological data were extracted, which enriched the information of origin tracing. Through conventional gemmological tests and chemical composition tests, it was determined that the orange-yellow garnet from Zambia is spessartine with a terminal component content of up to 92 mol.%. The test results of Raman spectroscopy and infrared spectroscopy showed that the three characteristic Raman peaks of spessartine are located near 907, 551 cm-1 and 349 cm-1. The characteristic infrared bands are near 976, 891, 865, 629, 571, 522 cm-1. By analyzing the attribution of UV-Vis absorption spectrum peaks of the spessartine samples from Zambia, the orange-yellow colour of the spessartine is caused by Mn2+ and Fe2+, and the corresponding absorption peaks are at 409, 421, 430, 460, 482 nm and 504, 525, 570 nm.

     

/

返回文章
返回