淬火天然与合成紫黄晶显微中红外光谱研究  

The Micro Mid-Infrared Spectral Study on Quench of Natural and Synthetic Ametrine

作　　者：邵天 罗泽敏[1] 陈涛[1] 沈锡田 SHAO Tian;LUO Ze-min;CHEN Tao;Andy Hsitien Shen

机构地区：[1]中国地质大学珠宝学院,湖北武汉430074

出　　处：《光谱学与光谱分析》2018年第9期2749-2756,共8页Spectroscopy and Spectral Analysis

基　　金：国家自然科学基金面上项目(41572033);湖北省自然科学基金项目(2014CFB347);中国地质大学(武汉)珠宝检测技术创新中心科研项目(CIGTXM-201512S)资助

摘　　要：紫黄晶是珍贵的水晶变种,其紫-黄色区域分别具有特征的中红外吸收光谱,在不同温度具有不同变化规律,这些规律无法在单次、单点实验中加以总结。实验通过热处理和显微红外光谱技术,对不同温度淬火紫黄晶的紫-黄色区进行线扫描,分析一系列温度、空间变化下的中红外光谱,实验表明水对于紫黄晶的颜色影响不大,在加热过程中谱线会发生规律性变化。紫色区3 585和3 614cm^(-1)尖锐峰、3 400cm^(-1)附近宽泛峰同时变化表明宝石在受热过程以结构水变化为主,而受热后紫色区的特征峰减弱及黄区特征峰增强的现象可能与结构水中H+或其他阳离子的移动有关。同时发现对于热处理产生的黄晶,中红外光谱仍保持紫晶特征吸收光谱。Ametrine is the valuable variety in alpha quartz,and its mid-Infrared(MIR)spectra research helps to understand the differences of violet and yellow zones in amtrine.The natural and synthetic ametrine have the specific MIR absorptionspectra in the violet-yellow color zones respectively.When quenched under thedifferent temperatures,the spectra can change regularly.We conducted quenchexperiments of natural and synthetic ametrine using tube furnace and collectedthe micro MIR spectra of natural and synthetic ametrine under different quench temperature in the violet-yellow color zones.The experiments suggested that water had not direct correlation to do with the color.In sharps peak at 3 585 and3 614 cm-1 of violet zone and broad band near 3 400 cm-1 of yellowzone,the simultaneous changes of these peaks,which occurred in same temperature,indicating that when the samples heated,the structural water may play a dominant role in change.During the heat treatment,the peaks decreased in violet zone while increased in yellow zone,that could be explained by the migration of H+or other positive ions through the structure channels of alpha-quartz.Atthe same time,the research pointed out that the MIR spectra of heated yellow quartz is largely similar to the amethyst one.

关 键 词：紫黄晶 显微红外光谱 热处理 结构水 

分 类 号：P575.4[天文地球—矿物学]