{"title":"地质材料无损微x射线荧光定量分析","authors":"Jinhua Li","doi":"10.46770/as.2022.112","DOIUrl":null,"url":null,"abstract":": Micro X-ray fluorescence (µXRF) is an atomic spectroscopy for analyzing micro areas of a sample using Xray beams and mapping elemental distribution on the sample by spectrum acquisition at individual pixel positions. We have examined the potential of rapid and non-destructive µXRF analysis to quantitatively determine the chemical composition of geological samples by correcting standardless fundamental parameters (SFP) quantification data. Based on analysis and comparison of a set of certified international standard silicate glass, linear relationships between μXRF SFP quantification data and certified values of Na 2 O, MgO, Al 2 O 3 , SiO 2 , K 2 O, CaO, TiO 2 , MnO, and FeO were developed, and the corresponding calibration equations were calculated. Further tests on flat or uneven homogeneous glass demonstrated that calibrated results of all major elements were similar with certified values, with improved accuracy of ~10%. Analysis of typical geological materials, including pure minerals, heterogeneous basaltic rock, and micro areas, indicated calibrated results were closer to certified/reference values for most elements. This study reveals that µXRF is a promising technique for rapid, non-destructive, and quantitative investigation of chemical composition of specimens at the microscale level. µXRF measurements and calibration equations developed in this study could be used to rapidly characterize geological materials and non-destructively analyze precious extraterrestrial materials.","PeriodicalId":8642,"journal":{"name":"Atomic Spectroscopy","volume":null,"pages":null},"PeriodicalIF":3.4000,"publicationDate":"2022-09-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Non-Destructive Micro X-Ray Fluorescence Quantitative Analysis Of Geological Materials\",\"authors\":\"Jinhua Li\",\"doi\":\"10.46770/as.2022.112\",\"DOIUrl\":null,\"url\":null,\"abstract\":\": Micro X-ray fluorescence (µXRF) is an atomic spectroscopy for analyzing micro areas of a sample using Xray beams and mapping elemental distribution on the sample by spectrum acquisition at individual pixel positions. We have examined the potential of rapid and non-destructive µXRF analysis to quantitatively determine the chemical composition of geological samples by correcting standardless fundamental parameters (SFP) quantification data. Based on analysis and comparison of a set of certified international standard silicate glass, linear relationships between μXRF SFP quantification data and certified values of Na 2 O, MgO, Al 2 O 3 , SiO 2 , K 2 O, CaO, TiO 2 , MnO, and FeO were developed, and the corresponding calibration equations were calculated. Further tests on flat or uneven homogeneous glass demonstrated that calibrated results of all major elements were similar with certified values, with improved accuracy of ~10%. Analysis of typical geological materials, including pure minerals, heterogeneous basaltic rock, and micro areas, indicated calibrated results were closer to certified/reference values for most elements. This study reveals that µXRF is a promising technique for rapid, non-destructive, and quantitative investigation of chemical composition of specimens at the microscale level. µXRF measurements and calibration equations developed in this study could be used to rapidly characterize geological materials and non-destructively analyze precious extraterrestrial materials.\",\"PeriodicalId\":8642,\"journal\":{\"name\":\"Atomic Spectroscopy\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":3.4000,\"publicationDate\":\"2022-09-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Atomic Spectroscopy\",\"FirstCategoryId\":\"92\",\"ListUrlMain\":\"https://doi.org/10.46770/as.2022.112\",\"RegionNum\":2,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SPECTROSCOPY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atomic Spectroscopy","FirstCategoryId":"92","ListUrlMain":"https://doi.org/10.46770/as.2022.112","RegionNum":2,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SPECTROSCOPY","Score":null,"Total":0}
Non-Destructive Micro X-Ray Fluorescence Quantitative Analysis Of Geological Materials
: Micro X-ray fluorescence (µXRF) is an atomic spectroscopy for analyzing micro areas of a sample using Xray beams and mapping elemental distribution on the sample by spectrum acquisition at individual pixel positions. We have examined the potential of rapid and non-destructive µXRF analysis to quantitatively determine the chemical composition of geological samples by correcting standardless fundamental parameters (SFP) quantification data. Based on analysis and comparison of a set of certified international standard silicate glass, linear relationships between μXRF SFP quantification data and certified values of Na 2 O, MgO, Al 2 O 3 , SiO 2 , K 2 O, CaO, TiO 2 , MnO, and FeO were developed, and the corresponding calibration equations were calculated. Further tests on flat or uneven homogeneous glass demonstrated that calibrated results of all major elements were similar with certified values, with improved accuracy of ~10%. Analysis of typical geological materials, including pure minerals, heterogeneous basaltic rock, and micro areas, indicated calibrated results were closer to certified/reference values for most elements. This study reveals that µXRF is a promising technique for rapid, non-destructive, and quantitative investigation of chemical composition of specimens at the microscale level. µXRF measurements and calibration equations developed in this study could be used to rapidly characterize geological materials and non-destructively analyze precious extraterrestrial materials.
期刊介绍:
The ATOMIC SPECTROSCOPY is a peer-reviewed international journal started in 1962 by Dr. Walter Slavin and now is published by Atomic Spectroscopy Press Limited (ASPL). It is intended for the rapid publication of both original articles and review articles in the fields of AAS, AFS, ICP-OES, ICP-MS, GD-MS, TIMS, SIMS, AMS, LIBS, XRF and related techniques. Manuscripts dealing with (i) instrumentation & fundamentals, (ii) methodology development & applications, and (iii) standard reference materials (SRMs) development can be submitted for publication.