Gemmological and Chemical Characteristics of Spessartine from Zambia

Zhang Haikun, Liu Cuihong, Song Qiurong, A. Shen
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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.
赞比亚spessartiine的宝石学和化学特征
赞比亚的伦达齐地区是一个相对较新的豆芽菜产地。本文对该地区的一批橙黄色石榴石样品进行了化学成分、宝石学和光谱特征的系统研究。提取了有意义的宝石学数据,丰富了产地溯源信息。通过常规的宝石学检测和化学成分检测,确定产自赞比亚的橙黄色石榴石为spessartine,终组分含量高达92 mol.%。拉曼光谱和红外光谱测试结果表明,spessmartine的三个特征拉曼峰位于907、551和349 cm-1附近。特征红外波段在976、891、865、629、571、522 cm-1附近。通过对赞比亚spessartine样品紫外可见吸收光谱峰的归属分析,spessartine的橘黄色是由Mn2+和Fe2+引起的,对应的吸收峰位于409、421、430、460、482 nm和504、525、570 nm。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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