岩矿测试
巖礦測試
암광측시
Rock and Mineral Analysis
2015年
5期
544-549
,共6页
严俊%刘晓波%王巨安%方飚%刘培钧%杨彬彬
嚴俊%劉曉波%王巨安%方飚%劉培鈞%楊彬彬
엄준%류효파%왕거안%방표%류배균%양빈빈
仿制绿松石%矿物组成%傅里叶变换红外光谱法%X射线粉晶衍射法%X射线荧光光谱法
倣製綠鬆石%礦物組成%傅裏葉變換紅外光譜法%X射線粉晶衍射法%X射線熒光光譜法
방제록송석%광물조성%부리협변환홍외광보법%X사선분정연사법%X사선형광광보법
imitated turquoise%mineral composition%Fourier Transform Infrared Spectroscopy(FTIR )%X-ray Diffraction(XRD)%X-ray Fluorescence Spectroscopy(XRF)
近年来绿松石及其仿制品的鉴定工作较多局限于应用傅里叶变换红外光谱对仿制品进行简单的筛选,前人报道的仿制绿松石的矿物组成主要为单一的矿物相(如异极矿、三水铝石、磷铝石、羟硅硼钙石、菱镁矿等)。本文应用傅里叶变换红外光谱( FTIR)、X射线粉晶衍射( XRD)与X射线荧光光谱( XRF)对当前珠宝市场上几种新型仿制绿松石进行了初步分类,并对不同类别的仿制绿松石的具体矿物组成、物相及晶型特征作了对比研究。结果表明,这些新型仿制绿松石可分为三大类:一类主要由硅酸盐(斜硅钙石)与碳酸盐(方解石)两种矿物组成;另一类为白云石与方解石两种碳酸盐矿物的混合相;第三类以硅酸盐类为主要矿物,并含有钡长石、辉石与石英。显然,新型仿制绿松石的矿物组成明显相异于传统仿制品,可见仿制绿松石的矿物组成日趋多样性、复杂化,该现状必然对新型仿制样品的物相鉴定提出了更高的要求。
近年來綠鬆石及其倣製品的鑒定工作較多跼限于應用傅裏葉變換紅外光譜對倣製品進行簡單的篩選,前人報道的倣製綠鬆石的礦物組成主要為單一的礦物相(如異極礦、三水鋁石、燐鋁石、羥硅硼鈣石、蔆鎂礦等)。本文應用傅裏葉變換紅外光譜( FTIR)、X射線粉晶衍射( XRD)與X射線熒光光譜( XRF)對噹前珠寶市場上幾種新型倣製綠鬆石進行瞭初步分類,併對不同類彆的倣製綠鬆石的具體礦物組成、物相及晶型特徵作瞭對比研究。結果錶明,這些新型倣製綠鬆石可分為三大類:一類主要由硅痠鹽(斜硅鈣石)與碳痠鹽(方解石)兩種礦物組成;另一類為白雲石與方解石兩種碳痠鹽礦物的混閤相;第三類以硅痠鹽類為主要礦物,併含有鋇長石、輝石與石英。顯然,新型倣製綠鬆石的礦物組成明顯相異于傳統倣製品,可見倣製綠鬆石的礦物組成日趨多樣性、複雜化,該現狀必然對新型倣製樣品的物相鑒定提齣瞭更高的要求。
근년래록송석급기방제품적감정공작교다국한우응용부리협변환홍외광보대방제품진행간단적사선,전인보도적방제록송석적광물조성주요위단일적광물상(여이겁광、삼수려석、린려석、간규붕개석、릉미광등)。본문응용부리협변환홍외광보( FTIR)、X사선분정연사( XRD)여X사선형광광보( XRF)대당전주보시장상궤충신형방제록송석진행료초보분류,병대불동유별적방제록송석적구체광물조성、물상급정형특정작료대비연구。결과표명,저사신형방제록송석가분위삼대류:일류주요유규산염(사규개석)여탄산염(방해석)량충광물조성;령일류위백운석여방해석량충탄산염광물적혼합상;제삼류이규산염류위주요광물,병함유패장석、휘석여석영。현연,신형방제록송석적광물조성명현상이우전통방제품,가견방제록송석적광물조성일추다양성、복잡화,해현상필연대신형방제양품적물상감정제출료경고적요구。
Identification of turquoises and corresponding imitations is commonly determined by Fourier Transform Infrared( FTIR)Spectrometer. Previous studies have shown that imitation turquoise was mainly composed of a single mineral phase such as hemimorphite,gibbsite,variscite,hydroxyl datolite,or magnesite. Fourier Transform Infrared (FTIR)Spectroscopy,X-ray Diffraction(XRD)and X-ray Fluorescence Spectroscopy(XRF)were used to investigate new imitated turquoises in order to classify them based on their mineral compositions and the method is described in this paper. Mineral compositions,crystal phases and crystalline appearance of different types of imitated turquoises were also compared. Results show that new imitated turquoises in this study can be mainly classified into three groups. The first group is mainly composed of silicate( larnite)and carbonate( calcite). The second group is composed of mixtures of calcite and dolomite. The third group consists of silicate,and minor barium feldspar, pyroxene and quartz. The mineral compositions of new imitated turquoises were significantly different from those of traditional imitations. In other words,the mineral compositions of imitated turquoises are becoming more diverse and complicated,which implies a higher demand for jewelry inspection agencies and researchers.