红外技术
紅外技術
홍외기술
INFRARED TECHNOLOGY
2015年
2期
171-175
,共5页
徐志%李锐%郭倩%曹姝旻
徐誌%李銳%郭倩%曹姝旻
서지%리예%곽천%조주민
红外光谱%镜面反射%文石晶体%晶体取向
紅外光譜%鏡麵反射%文石晶體%晶體取嚮
홍외광보%경면반사%문석정체%정체취향
infrared spectroscopy%spectral reflection%aragonite crystal%crystal orientation
采用傅里叶变换红外光谱仪KBr粉末压片法和原物镜面反射法对8件文石样品进行测试,对比了两种方法的差异。深入探讨文石晶体在不同方向上红外镜面反射光谱的变化,发现文石的红外镜面反射光谱具有显著的各向异性:在垂直、平行和斜交于文石 c 轴的面上[CO3]2-产生的 v3振动反射峰宽化易出现变形和位移现象;v2振动反射峰峰位和相对强度发生明显的规律性变化。由此,认为红外镜面反射光谱可用于文石晶体取向的研究。在此基础上,对5件养殖珍珠表面和剖面进行测试对比。结果显示,从养殖珍珠表面获得的红外镜面反射谱与文石垂直于c轴的底面所得相同;养殖珍珠剖面上测得的红外镜面反射谱与文石平行/斜交于c轴的面所得谱类似,于是推断养殖珍珠中文石晶体是以c轴指向球心的方式排列的。
採用傅裏葉變換紅外光譜儀KBr粉末壓片法和原物鏡麵反射法對8件文石樣品進行測試,對比瞭兩種方法的差異。深入探討文石晶體在不同方嚮上紅外鏡麵反射光譜的變化,髮現文石的紅外鏡麵反射光譜具有顯著的各嚮異性:在垂直、平行和斜交于文石 c 軸的麵上[CO3]2-產生的 v3振動反射峰寬化易齣現變形和位移現象;v2振動反射峰峰位和相對彊度髮生明顯的規律性變化。由此,認為紅外鏡麵反射光譜可用于文石晶體取嚮的研究。在此基礎上,對5件養殖珍珠錶麵和剖麵進行測試對比。結果顯示,從養殖珍珠錶麵穫得的紅外鏡麵反射譜與文石垂直于c軸的底麵所得相同;養殖珍珠剖麵上測得的紅外鏡麵反射譜與文石平行/斜交于c軸的麵所得譜類似,于是推斷養殖珍珠中文石晶體是以c軸指嚮毬心的方式排列的。
채용부리협변환홍외광보의KBr분말압편법화원물경면반사법대8건문석양품진행측시,대비료량충방법적차이。심입탐토문석정체재불동방향상홍외경면반사광보적변화,발현문석적홍외경면반사광보구유현저적각향이성:재수직、평행화사교우문석 c 축적면상[CO3]2-산생적 v3진동반사봉관화역출현변형화위이현상;v2진동반사봉봉위화상대강도발생명현적규률성변화。유차,인위홍외경면반사광보가용우문석정체취향적연구。재차기출상,대5건양식진주표면화부면진행측시대비。결과현시,종양식진주표면획득적홍외경면반사보여문석수직우c축적저면소득상동;양식진주부면상측득적홍외경면반사보여문석평행/사교우c축적면소득보유사,우시추단양식진주중문석정체시이c축지향구심적방식배렬적。
8 pieces of aragonite samples were tested with Fourier transform infrared spectrometer KBr powder tabletting and spectral reflection method, and the differences between the two methods are compared. The differences of IR spectral reflection spectrum from aragonite crystals different directions are discussed emphatically, and the difference is very significant in the vertical, parallel and oblique c-axis of aragonite crystals. The reflection peak that made by [CO3]2-v3widening will induce deformation and displacement; The peak position and relative strength ofv2 significantly changes regularly. Thus, the spectral reflection IR spectrum can be used in test of aragonite crystal orientation. On this basis, the surface and section of 5 pearls are used to compare. The results show that the spectral reflection IR spectrum measure from the pearl surface is same to that from aragonite bottom surface which is perpendicular to the c-axis, and that from the pearl section is similar to that from the plane parallel or oblique aragonite c-axis. Then, we can conclude that the aragonite in pearls is arranged by the way of crystal c-axis pointing to its core.