岩矿测试
巖礦測試
암광측시
ROCK AND MINERAL ANALYSIS
2009年
4期
361-363
,共3页
异性石%二价铁%平面四配位
異性石%二價鐵%平麵四配位
이성석%이개철%평면사배위
Eudialyte%Fe2+%planar four-fold coordination
对产于美国阿拉斯加的异性石的物理特性及化学成分进行分析.该异性石呈深红色,为一轴晶正光性;其紫外可见吸收光谱在530 nm处有明显的吸收带,在917 nm处有较弱的吸收带;穆斯堡尔谱及参数与俄罗斯科拉半岛深红色异性石和辽宁凤城深玫瑰色异性石相近;红外光谱特征与正光性异性石相似.探讨了该异性石的致色机理,认为其颜色主要与Fe2+有关,且异性石中的Fe2+主要以平面四配位存在.
對產于美國阿拉斯加的異性石的物理特性及化學成分進行分析.該異性石呈深紅色,為一軸晶正光性;其紫外可見吸收光譜在530 nm處有明顯的吸收帶,在917 nm處有較弱的吸收帶;穆斯堡爾譜及參數與俄囉斯科拉半島深紅色異性石和遼寧鳳城深玫瑰色異性石相近;紅外光譜特徵與正光性異性石相似.探討瞭該異性石的緻色機理,認為其顏色主要與Fe2+有關,且異性石中的Fe2+主要以平麵四配位存在.
대산우미국아랍사가적이성석적물리특성급화학성분진행분석.해이성석정심홍색,위일축정정광성;기자외가견흡수광보재530 nm처유명현적흡수대,재917 nm처유교약적흡수대;목사보이보급삼수여아라사과랍반도심홍색이성석화료녕봉성심매괴색이성석상근;홍외광보특정여정광성이성석상사.탐토료해이성석적치색궤리,인위기안색주요여Fe2+유관,차이성석중적Fe2+주요이평면사배위존재.
The eudialyte from Alaska is crimson and optically positive. Optical absorption spectra of the eudialyte are characterized by obvious absorption band at 530 nm and weak absorption band at 917 nm. Its physical properties, chemical composition and Mossbauer spectrum are similar to the crimson eudialyte from Kola peninsula in Russia and the deep Rose eudialyte from Fengcheng in Liaoning province. And its infra-red spectrum is similar to that of the optically positive eudialyte. According to research of E. V. Pol' shin and Hanxueming, author thinks the colour of the eudialyte from Alaska is related to Fe2+ and Fe2+ in the eudialyte is mainly in a planar four-fold coordination.