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激光剥蚀-等离子体质谱技术及其在地球化学宇宙化学和环境研究中的应用
引用本文:JOCHUM Klaus Peter,STOLL Brigitte,FRIEDRICH Jon M,AMINI Marghaleray,BECKER Stefan,DüCKING Marc,EBEL Denton S,ENZWEILER Jacinta,胡明月,KUZMIN Dmitry,MERTZ KRAUS Regina,MüLLER Werner E G,REGNERY Julia,SOBOLEV Alexander,王晓红,詹秀春. 激光剥蚀-等离子体质谱技术及其在地球化学宇宙化学和环境研究中的应用[J]. 岩矿测试, 2009, 28(1): 53-68
作者姓名:JOCHUM Klaus Peter  STOLL Brigitte  FRIEDRICH Jon M  AMINI Marghaleray  BECKER Stefan  DüCKING Marc  EBEL Denton S  ENZWEILER Jacinta  胡明月  KUZMIN Dmitry  MERTZ KRAUS Regina  MüLLER Werner E G  REGNERY Julia  SOBOLEV Alexander  王晓红  詹秀春
作者单位: 
摘    要:激光剥蚀-等离子体质谱(LA-ICPMS)已成为地球化学、宇宙化学和环境研究领域元素和同位素原位分析最重要的技术之一。文章介绍了多种类型的质谱仪及其使用的激光器。用途最广的LA-ICPMS仪器之一是单接收器扇形磁场质谱仪,配有Nd:YAG激光剥蚀系统(激光波长分为193 nm和213 nm两种),MPI Mainz实验室使用的就是这套系统,文章对此作一详细介绍。文中阐述了数据优化技术及其多种校正过程;介绍LA-ICPMS在痕量元素和同位素分析领域的一些应用,包括参考物质的研制,Hawaiian玄武岩、Martian陨石、生物骨针和珊瑚虫中痕量元素分析及熔融包裹体和富钙-铝碳质球粒陨石中的铅和锶同位素测量。

关 键 词:激光剥蚀-等离子体质谱  地质样品  参考物质  陨石  生物样品  痕量元素  同位素比值
收稿时间:2008-09-27
修稿时间:2008-10-26

Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry and Its Application in Geochemistry, Cosmochemistry and Environmental Research
JOCHUM Klaus Peter,STOLL Brigitte,FRIEDRICH Jon M,AMINI Marghaleray,BECKER Stefan,DüCKING Marc,EBEL Denton S,ENZWEILER Jacinta,HU Ming-yue,KUZMIN Dmitry,MERTZ-KRAUS Regina,MüLLER Werner E G,REGNERY Julia,SOBOLEV Alexander,WANG Xiao-hong,ZHAN Xiu-chun. Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry and Its Application in Geochemistry, Cosmochemistry and Environmental Research[J]. Rock and Mineral Analysis, 2009, 28(1): 53-68
Authors:JOCHUM Klaus Peter  STOLL Brigitte  FRIEDRICH Jon M  AMINI Marghaleray  BECKER Stefan  DüCKING Marc  EBEL Denton S  ENZWEILER Jacinta  HU Ming-yue  KUZMIN Dmitry  MERTZ-KRAUS Regina  MüLLER Werner E G  REGNERY Julia  SOBOLEV Alexander  WANG Xiao-hong  ZHAN Xiu-chun
Affiliation:[1]Max Planck-lnstitut for Chemie, Mainz 55020, Germany [2]Department of Earth and Planetary Sciences, American Museum of Natural History, New York 10024, USA [3]Department of Chemistry, Fordham University, Bronx,New York 10458, USA [4]Saskatchewan Isotope Laboratory, Department of Geological Sciences, University of Saskatchewan, Saskatoon S7N 5E2, Canada [5]Bundeskriminalamt, Wiesbaden 65173, Germany [6]Instituto de Geoci6ncias, University of Campinas, CP 6152 Campinas, CEP 13083-970, Brazil [7]National Research Center for Geoanalysis, Beijing 100037, China [8]Institut for Geowissenschaften, Universitat Mainz, Mainz 55099, Germany [9]Institut for Physiologische Chemie, Universitat Mainz, Mainz 55099, Germany [10]Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, Novosibirsk 630090, Russia [11]V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow 119991, Russia
Abstract:Laser ablation (LA)-inductively coupled plasma-mass spectrometry (ICP-MS) has become one of the most important methods for in situ trace elemental and isotopic analysis in geochemistry, cosmochemistry and environmental research. For these purposes, different kinds of mass spectrometers and lasers are used, which are presented in this paper. One of the most useful LA-ICPMS instruments is the combination of a single-collector sector field mass spectrometer with Nd:YAG laser ablation systems (193 nm and 213 nm wavelengths, respectively). This design used in the MPI Mainz laboratory is described in detail in this paper. Data optimization techniques including diverse correction procedures are also discussed. To demonstrate the power of LA-ICPMS, several applications of trace elemental and isotopic analysis are presented, such as investigations of reference materials, trace element analysis in Hawaiian basalts, Martian meteorites, biological spicules and corals, as well as Pb and Sr isotope measurements of melt inclusions and Ca-Al rich inclusions of carbonaceous chondrites.
Keywords:laser ablation-inductively coupled plasma-mass spectrometry(LA-ICPMS)  geological sample  reference material  meteorite  biological sample  trace element  isotope ratio
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