肯尼亚西南部红宝石的谱学及成分特征研究

Spectral Characteristic and Chemical Composition of Ruby from Southwest Kenya

  • 摘要: 近年来非洲肯尼亚红宝石在国际彩色宝石市场具有一定占有率, 目前其谱学及成分特征等资料仍有待补充。本文以肯尼亚西南边境产出的40粒红宝石样品作为研究对象,采用常规宝石学仪器、傅里叶红外光谱仪、显微激光拉曼光谱仪、紫外-可见分光光度计和激光剥蚀等离子体质谱仪等测试仪器对该产地红宝石样品的宝石学性质、谱学特征和化学成分特征进行系统研究,旨在探讨肯尼亚该矿区红宝石谱学特征和化学成分特征,为红宝石的产地溯源提供数据。研究结果表明,该产地红宝石样品的折射率为1.759~1.778,双折射率为0.009~0.010,相对密度为3.95~4.01,短波紫外光下呈无-弱荧光,长波紫外光下呈弱-中等红色荧光;样品中所含的硬水铝石、金红石、铬铁矿、角闪石、磷灰石、云母等包裹体未见热处理迹象;样品化学成分主量Al2O3的含量为95.8%~97.1%,微量元素具高Cr、中Fe、低V的特征,红色调饱和度与Cr元素含量正相关,利用Fe、Cr、V、Ga四个元素可以与其他红宝石产地区分;样品颜色色调为红色-紫红色,颜色饱和度级别大多数在艳红-浓红区间,其中艳红(鸽血红)比例约占40%。

     

    Abstract: Rubies from Kenya in Africa currently occupy a significant portion of the color-stone market, there are still needs for additional spectral characteristic and chemical composition information. In this study, the gemmological characteristics and chemical compositions of 40 pieces of ruby samples from southwest Kenya were investigated by conventional gemmological test instruments, FTIR spectrometer, Raman spectrometer, laser ablation inductively coupled plasma mass spectrometer(LA-ICP-MS), ultraviolet-visible spectrometer(UV-Vis), and other test instruments, to explore the spectral characteristics and chemiacal compositions of the ruby samples from southwest Kenya, and to provide data for the origin identification of ruby. The results show that the refractive index of the ruby sample is 1.759 to 1.778, the birefringence is 0.009 to 0.010, and the relative density is 3.95 to 4.01. The ruby samples show weak to medium red fluorescence under long-wave ultraviolet fluorescence and none to weak fluorescence under short-wave ultraviolet fluorescence. The ruby samples contain inclusions included diaspore, rutile, chromite, amphibole, apatite and mica. These inclusions show no sign of heat treatment. The content of Al2O3 of the ruby samples range from 95.8% to 97.1%, the trace elements show high Cr, medium Fe and low V featurs. There is a positive correlation between the saturation of red and the contents of Cr. The contents of Fe, Cr, V, Ga could distinguish ruby samples from southwest Kenya with rubies from other origins. The hue of the ruby samples are red to purplish red, the saturation mainly ranges from vivid red to intense red. The proportion of vivid red ("Pigeon's blood" red) are about 40% of ruby samples from Kenya.

     

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