期刊文献+

合成镁橄榄石的矿物学研究 被引量:5

Study on the Mineralogy of Synthetic Forsterite
下载PDF
导出
摘要 人工合成的镁橄榄石具有优越的物理化学性能,使其在诸多领域得到应用,其中蓝紫色合成镁橄榄石被用作坦桑石的替代品进入珠宝市场,引起了珠宝行内外的广泛关注。本文通过X射线荧光光谱的定量分析和紫外-可见光吸收光谱的颜色成因分析,得出人工合成的蓝紫色镁橄榄石的主要成分为MgO和SiO2,并添加了致色金属元素钴和钒,组份相对简单,蓝紫色调的产生与钴离子有关;对合成橄榄石、天然橄榄石和坦桑石进行拉曼光谱(785nm)的定性分析,得到合成镁橄榄石与天然橄榄石都具有特征Si-O伸缩振动引起的拉曼位移820cm-1、853cm-1和961cm-1,而坦桑石中存在特征Si-O伸缩振动引起的拉曼位移866cm-1、923cm-1和1148cm-1,可有效鉴定该三种矿物。 Synthetic forsterites are widely used in many fields because of the super physical and chemical property. Among them the blue and purple ones were used as substitutes for zoisites in the gemstone market, which arose the common attentions in and around the gemstone industry. This paper was based on quantitative analyzing tested by XRF and coloration mechanism study tested by UV-VIS absorption spectrum, it was found that the main components of synthetic blue and purple forsterite were MgO and SiO2,and coloration element Co and V were added in it, the components were fewer; The turn-up of blue and purple color was connecting with Co ion; via qualitative analysis on synthetic forsterite, natural peridot and zoisite tested by Raman specter, it was found that Raman shifts 820cm^-1, 853cm^-1 and 961cm^-1 belonged to diagnostic stretching vibration of band Si-O existed in the Raman spectra of synthetic forsterite and peridot, whereas Raman shifts 866cm^-1 , 923cm^-1 and 1148cm^-1 belonged to diagnostic stretching vibration of band Si-O existed in the Raman spectra of zoisite. Owing to above testing methods, synthetic forsterite could be identified effectively with natural peridot and zoisite.
出处 《人工晶体学报》 EI CAS CSCD 北大核心 2007年第6期1431-1434,共4页 Journal of Synthetic Crystals
关键词 镁橄榄石 坦桑石 橄榄石 X射线荧光光谱 紫外-可见光吸收光谱 拉曼光谱 forsterite zoisite peridot XRF UV-VIS absorption spectrum Raman spectrum
  • 相关文献

参考文献5

二级参考文献16

  • 1吴国学,李守义,李书法,陈国华.不同石英脉型金银矿床中含矿石英脉的红外光谱对比[J].吉林大学学报(地球科学版),2004,34(4):527-530. 被引量:3
  • 2魏存弟,赵峰,马鸿文,李金洪,杨殿范,三国彰.叶蜡石加热相变及其演化特征[J].吉林大学学报(地球科学版),2005,35(2):150-154. 被引量:13
  • 3宋茂双,谢鸿森,徐有生.地幔物质的性质、状态与演化及相变动力学研究进展[J].地质地球化学,1995,23(6):76-79. 被引量:3
  • 4Fujimori H,Komatsu H,Loku K,et al.Anharmonic lattice mode of Ca2SiO4 ultraviolet laser Raman spectroscopy at high temperatures[J].Phys Rev B,2002,66:64 306-64 311.
  • 5Merkel S,Goncharov A F,Mao H-K,et al.Raman spectroscopy of iron to 152 Gigapascals:Implications for earth's inner core[J].Science,2000,288:1 626-1 630.
  • 6Dan J Durben,Paul F Mcmillan,George H Wolf.Raman study of the high-pressure behavior of forsterite(Mg2SiO4) crystal and glass[J].American Mineralogist,1993,78:1 143-1 148.
  • 7Lin C C.High-pressure Raman spectroscopic study of Co-and Ni-olivines[J].Physics Chemistry Minerals,2001,28:249-257.
  • 8Downs Rorert T,Zha Chang Sheng,Duffy Thomas S,et al.The equation of state of forsterite to 17.2 GPa and effects of pressure media[J].American Mineralogist,1996,81:51-55.
  • 9Pui K Lam,Rici Yu,Matthew W Lee.Structural distortions and vibrational modes in Mg2SiO4[J].American Mineralogist,1990,75:109-119.
  • 10Wang S Y,Sharma S K,Cooney T F.Micro-Raman and infrared spectral study of forsterite under high pressure[J].American Mineralogist,1993,78:469-476.

共引文献7

同被引文献235

引证文献5

二级引证文献52

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部