Professional Committee of Rock and Mineral Testing Technology of the Geological Society of China, National Geological Experiment and Testing CenterHost
2018 Vol. 37, No. 1
Article Contents

Chuan-bo XIA, Xue-hai CHENG, Hui-tang ZHANG, Wei ZHAO, Qing WANG. Determination of Twelve Major and Minor Elements in Tourmaline by X-ray Fluorescence Spectrometry with Fusion Sample Preparation[J]. Rock and Mineral Analysis, 2018, 37(1): 36-42. doi: 10.15898/j.cnki.11-2131/td.201610260197
Citation: Chuan-bo XIA, Xue-hai CHENG, Hui-tang ZHANG, Wei ZHAO, Qing WANG. Determination of Twelve Major and Minor Elements in Tourmaline by X-ray Fluorescence Spectrometry with Fusion Sample Preparation[J]. Rock and Mineral Analysis, 2018, 37(1): 36-42. doi: 10.15898/j.cnki.11-2131/td.201610260197

Determination of Twelve Major and Minor Elements in Tourmaline by X-ray Fluorescence Spectrometry with Fusion Sample Preparation

  • Tourmaline is a class of boron-bearing aluminosilicate minerals. It has a complex chemical component and stable chemical property, and is difficult to decompose by wet methods. The high content of B2O3 makes it difficult to simultaneously determine major and minor elements in tourmaline. X-ray Fluorescence Spectrometry (XRF) was applied to determine Na2O, MgO, Al2O3, SiO2, P2O5, K2O, CaO, TiO2, V2O5, Cr2O, MnO, TFe2O3 in tourmaline samples with fusion sample preparation in this study. The dilution ratio of 1:10 was set for the sample to flux lithium tetraborate-lithium metaborate-lithium fluoride (quality ratio of 4.5:1:0.4) in order to eliminate the particle size effect and mineral effect. When the tourmaline reference materials were unavailable, soil, stream sediment and different types of rock reference materials were used to establish calibration curves. The accuracy of the method was verified using reference materials that have chemical compositions similar to tourmaline. The relative standard deviation (RSD, n=11) was less than 4.2%. The proposed method was used to determine four different tourmaline samples, the results were in good agreement with the values obtained by wet chemical methods. This method solved the problem that tourmaline is difficult to decompose and eliminated the interference effect of boron. The analytical results are accurate and reliable. Compared with other methods, this method is easy to operate and has a short analytical time.
  • 加载中
  • [1] 胡应模, 陈旭波, 汤明茹.电气石功能复合材料研究进展及前景展望[J].地学前缘, 2014, 21(5):331-337.

    Google Scholar

    Hu Y M, Chen X B, Tang M R.Research development and prospects of functional tourmaline composites[J].Earth Science Frontiers, 2014, 21(5):331-337.

    Google Scholar

    [2] 黄雪飞, 张宝林, 李晓利, 等.电气石研究进展及其找矿意义[J].黄金科学技术, 2012, 20(3):56-65.

    Google Scholar

    Huang X F, Zhang B L, Li X L, et al.Research progress of tourmaline and its prospecting significance[J].Gold Science & Technology, 2012, 20(3):56-65.

    Google Scholar

    [3] Hinsberg V J V, Henry D J, Marschall H R.Tourmaline:An ideal indicator of its host environment[J].Canadian Mineralogist, 2011, 49(1):1-16. doi: 10.3749/canmin.49.1.1

    CrossRef Google Scholar

    [4] 岩石矿物分析编委会.岩石矿物分析(第四版第二分册)[M].北京:地质出版社, 2011:390-396.

    Google Scholar

    The Editorial Committee of Rock and Mineral Analysis.Rock and Mineral Analysis (Fourth Edition:Volume Ⅱ)[M].Beijing:Geological Publishing House, 2011:390-396.

    Google Scholar

    [5] King R W, Kerrich R W, Daddar R.REE distributions in tourmaline:An INAA technique involving pretreatment by B volatilization[J].American Mineralogist, 1988, 73:424-431.

    Google Scholar

    [6] de Oliveira E F, Lacerda M A S, Amaral A M, et al. Chemical Composition of Tourmaline by Instrumental Neutron Activation Analysis[C]//Proceedings of International Nuclear Atlantic Conference-INAC 2005 Santos. Brazil, 2005.https://www.researchgate.net/publication/228450779_CHEMICAL_COMPOSITION_OF_TOURMALINES_BY_INSTRUMENTAL_NEUTRON_ACTIVATION_ANALYSIS

    Google Scholar

    [7] Aigbe S O, Ewa I O B, Ogunleye P O, et al.Elemental characterization of some Nigerian gemstones:Tourmaline, fluorite and topaz by instrumental neutron activation analysis[J].Journal of Radioanalytical & Nuclear Chemistry, 2013, 295(1):801-805.

    Google Scholar

    [8] 成学海, 夏传波, 郑建业, 等.封闭压力酸溶-电感耦合等离子体质谱法同时测定电气石中29种元素[J].岩矿测试, 2017, 36(3):231-238.

    Google Scholar

    Cheng X H, Xia C B, Zheng J Y, et al.Simultaneous determination of 29 trace elements in tourmaline samples by inductively coupled plasma mass spectrometry with pressurized acid decomposition[J].Rock and Mineral Analysis, 2017, 36(3):231-238.

    Google Scholar

    [9] Lihareva N, Kosturkova P, Vakarelska T.Application of sodium carbonate-zinc oxide decomposition mixture on ICP-AES determination of boron in tourmaline[J].Fresenius Journal of Analytical Chemistry, 2000, 367(1):84. doi: 10.1007/s002160051603

    CrossRef Google Scholar

    [10] Tamer K, Yusuf K, Shao Y J.Determination of tourma-line composition in pegmatite from Buldan, Denizli (Western Anatolia, Turkey) using XRD, XRF, and confocal Raman spectroscopy[J].Spectroscopy Letters, 2013, 46(7):499-506. doi: 10.1080/00387010.2012.760102

    CrossRef Google Scholar

    [11] Gullu B, Kadioglu Y K.Use of tourmaline as a potential petrogenetic indicator in the determination of host magma:CRS, XRD and PED-XRF methods[J].Spectrochimica Acta Part A:Molecular & Biomolecular Spectroscopy, 2017, 183:68.

    Google Scholar

    [12] 李国会, 李小莉.X射线荧光光谱分析熔融法制样的系统研究[J].冶金分析, 2015, 35(7):1-9.

    Google Scholar

    Li G H, Li X L.Systematic study on the fusion sample preparation in X-ray fluorescence spectrometric analysis[J].Metallurgical Analysis, 2015, 35(7):1-9.

    Google Scholar

    [13] Watanabe M.Sample preparation for X-ray fluorescence analysis Ⅳ.Fusion bead method-Part 1:Basic principles[J].Rigaku Journal, 2015, 32(2):12-17.

    Google Scholar

    [14] 周建辉, 白金峰.熔融玻璃片制样-X射线荧光光谱测定页岩中主量元素[J].岩矿测试, 2009, 28(2):179-181.

    Google Scholar

    Zhou J H, Bai J F.Determination of major elements in shale samples by X-ray fluorescence spectrometry with fused glass disc sample preparation[J].Rock and Mineral Analysis, 2009, 28(2):179-181.

    Google Scholar

    [15] 冯晓军.熔融制样-X射线荧光光谱法测定蛇纹石中主次组分[J].冶金分析, 2017, 37(4):27-32.

    Google Scholar

    Feng X J.Determination of major and minor components in serpentine by X-ray fluorescence spectrometry with fusion sample preparation[J].Metallurgical Analysis, 2017, 37(4):27-32.

    Google Scholar

    [16] Berryman E J, Kutzschbach M, Trumbull R B, et al.Tourmaline as a petrogenetic indicator in the Pfitsch Formation, Western Tauern Window, Eastern Alps[J].Lithos, 2017, 284-285:138-155. doi: 10.1016/j.lithos.2017.04.008

    CrossRef Google Scholar

    [17] 龚仓, 李高湖, 付桂花, 等.X射线荧光光谱法测定富砷地质样品中的主次痕量元素[J].分析试验室, 2014, 33(10):1220-1224.

    Google Scholar

    Gong C, Li G H, Fu G H, et al.Determination of major, minor and trace elements in geological samples with arsenic by X-ray fluorescence spectrometry[J].Chinese Journal of Analysis Laboratory, 2014, 33(10):1220-1224.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Tables(7)

Article Metrics

Article views(4423) PDF downloads(95) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint