中国地质学会岩矿测试技术专业委员会、国家地质实验测试中心主办

熔融制样-X射线荧光光谱法测定电气石中12种主次量元素

夏传波, 成学海, 张会堂, 赵伟, 王卿. 熔融制样-X射线荧光光谱法测定电气石中12种主次量元素[J]. 岩矿测试, 2018, 37(1): 36-42. doi: 10.15898/j.cnki.11-2131/td.201610260197
引用本文: 夏传波, 成学海, 张会堂, 赵伟, 王卿. 熔融制样-X射线荧光光谱法测定电气石中12种主次量元素[J]. 岩矿测试, 2018, 37(1): 36-42. doi: 10.15898/j.cnki.11-2131/td.201610260197
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

熔融制样-X射线荧光光谱法测定电气石中12种主次量元素

  • 基金项目:
    国土资源公益性行业科研专项(201311096)
详细信息
    作者简介: 夏传波, 硕士, 工程师, 主要从事岩石矿物中无机元素分析。E-mail:chuanbo007@126.com
  • 中图分类号: P578.953;O657.31

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

  • 电气石是一类含硼的铝硅酸盐矿物,化学成分复杂、化学稳定性强,不易湿法分解,B2O3含量较高,导致其主次量元素的同时测定存在一定困难。本文采用熔融法制样,建立了X射线荧光光谱法测定电气石Na2O、MgO、Al2O3、SiO2、P2O5、K2O、CaO、TiO2、V2O5、Cr2O3、MnO、TFe2O3等主次量元素的分析方法。样品与四硼酸锂-偏硼酸锂-氟化锂(质量比为4.5:1:0.4)混合熔剂的稀释比例为1:10,消除了粒度效应和矿物效应;在缺少电气石标准物质的情况下,选择土壤、水系沉积物及多种类型的地质标准物质绘制校准曲线,利用含量与电气石类似的标准物质验证准确度,测定结果的相对标准偏差小于4.2%。采用所建方法测定四种不同类型电气石实际样品,测定值与经典化学法基本吻合。本方法解决了电气石不易湿法分解和硼的干扰问题,测定结果准确可靠,与其他方法相比操作简便,分析周期短。
  • 加载中
  • 表 1  XRF仪器分析条件

    Table 1.  Working conditions of the XRF instrument

    元素 分析线 分析晶体 准直器 探测器 电压(kV) 电流(mA) 2θ (°) 背景(°) PHA
    LL UL
    Na RX25 S4 PC 55 60 47.492 48.900 100 350
    Mg RX25 S4 PC 55 60 39.060 40.500 100 350
    Al PET S4 PC 55 60 144.730 147.000 100 330
    Si PET S4 PC 55 60 109.042 111.000 100 320
    P Ge S4 PC 55 60 141.042 143.300 80 300
    K LiF1 S4 PC 55 60 136.588 139.500 100 300
    Ca LiF1 S4 PC 55 60 113.062 115.000 100 300
    Ti LiF1 S4 PC 55 60 86.106 88.500 100 320
    V LiF1 S4 PC 55 60 77.002 74.000 100 320
    Cr LiF1 S4 PC 55 60 69.306 74.000 130 320
    Mn LiF1 S4 SC 55 60 62.944 63.700 100 350
    Fe LiF1 S2 SC 55 60 57.476 58.800 80 350
    Br 1 LiF1 S2 SC 55 60 29.928 31.000 100 300
    Rh Rh-Kα1 LiF1 S2 SC 55 60 17.518 - 100 300
    Rh Rh-KαC LiF1 S2 SC 55 60 18.442 - 100 300
    注:均未使用滤光片, 衰减器均为1/1;Br用于校正Al的谱线重叠干扰;Rh为内标元素。
    下载: 导出CSV

    表 2  标准物质各元素含量范围

    Table 2.  Content range of elements in the certified reference materials

    元素 含量范围(%)
    Na2O 0.0066~13.77
    MgO 0.041~61.43
    Al2O3 0.053~38.62
    SiO2 0.62~98.51
    P2O5 0.0030~0.92
    K2O 0.0041~9.6
    CaO 0.052~40.39
    TiO2 0.0040~7.69
    V2O5 0.0004~0.14
    Cr2O3 0.0004~1.57
    MnO 0.0015~0.32
    TFe2O3 0.093~24.75
    下载: 导出CSV

    表 3  各组分校准曲线及基体校正

    Table 3.  Calibration curves of the components and matrix effect correction

    元素 校准曲线方程 相关系数 基体校正项 重叠校正项
    Na2O y=2.64274x-0.114574 0.9999 - -
    MgO y=0.930348x+0.0357911 0.9998 - -
    Al2O3 y=0.420649x-0.0226954 0.9999 Fe Br
    SiO2 y=0.423045x-2.27949 0.9992 Na, Mg, Ca -
    P2O5 y=0.144936x-0.000210712 0.9987 - -
    K2O y=0.0585628x-0.0343324 0.9997 - -
    CaO y=0.0650356x-0.001972964 0.9999 Mg Ti
    TiO2 y=0.0757955x-0.00999133 0.9997 Al -
    V2O5 y=0.0567832x+0.0102023 0.9976 - Ti
    Cr2O3 y=0.0296265x-0.0221646 0.9999 - V
    MnO y=0.0234417x-0.0037977 0.9966 Mg -
    TFe2O3 y=22.2998x-0.0147243 (0%~0.5%) 0.9908 Si, Al -
    y=20.5091x+0.128553 (0.5%~30%) 0.9997 Si, Al -
    注:y为组分含量(%),x为经校正后的计数率(kcps)或内标比;TFe2O3校准曲线是以Rh-KαC作内标,依据不同含量范围分段绘制校准曲线;“-”表示未作校正。
    下载: 导出CSV

    表 4  方法检出限

    Table 4.  Detection limits of the method

    元素 方法检出限(μg/g)
    计算值 测定值
    Na2O 102 426
    MgO 66 192
    Al2O3 103 156
    SiO2 21 180
    P2O5 16 25
    K2O 10 21
    CaO 13 21
    TiO2 9 27
    V2O5 5 23
    Cr2O3 3 15
    MnO 5 17
    TFe2O3 8 21
    下载: 导出CSV

    表 5  方法准确度

    Table 5.  Accuracy tests of the method

    元素 GBW07180 校准样品1 校准样品2
    本法(%) 推荐值(%) 本法(%) 推荐值(%) 本法(%) 推荐值(%)
    Na2O 0.034 0.040 2.03 2.03 1.83 1.81
    MgO 0.36 0.31 0.34 0.32 0.31 0.30
    Al2O3 43.37 42.97 33.91 33.99 38.02 38.11
    SiO2 38.89 39.03 49.86 49.61 45.19 44.96
    P2O5 0.14 0.14 0.15 0.15 0.16 0.16
    K2O 0.22 0.19 3.28 3.29 2.95 2.95
    CaO 0.096 0.12 1.15 1.14 1.07 1.06
    TiO2 1.83 2.06 1.17 1.29 1.32 1.49
    V2O5 0.011 0.013 - - - -
    Cr2O3 0.012 0.011 - - - -
    MnO 0.0016 0.0020 0.046 0.048 0.043 0.045
    TFe2O3 0.35 0.41 1.80 2.03 1.75 2.00
    注:“-”表示标准物质中该元素缺乏定值,未检测。
    下载: 导出CSV

    表 6  XRF分析不同制样方法的分析结果比对

    Table 6.  A comparison of analytical results of tourmaline samples measured by fusion and powder pellet preparation in XRF method

    元素 推荐值(%) 粉末压片法 本法(熔融法)
    测定值(%) 相对误差(%) 测定值(%) 相对误差(%)
    Na2O 2.43 2.22 -8.5 2.27 -6.6
    MgO 8.40 8.34 -0.8 8.49 1.1
    Al2O3 32.60 31.84 -2.3 32.76 0.5
    SiO2 36.24 35.36 -2.4 36.07 -0.5
    P2O5 0.14 0.19 35.7 0.15 7.1
    K2O 0.11 0.13 18.2 0.12 9.1
    CaO 0.55 0.72 30.2 0.59 7.3
    TiO2 0.62 0.59 -4.8 0.61 -1.6
    V2O5 0.027 0.036 32.0 0.026 -3.7
    Cr2O3 0.012 0.014 16.7 0.014 16.7
    MnO 0.024 0.030 20.8 0.025 4.2
    TFe2O3 5.07 5.32 4.9 5.16 1.8
    下载: 导出CSV

    表 7  本法与化学法的分析结果比对

    Table 7.  A comparison of analytical results of tourmaline samples measured by this method with chemical method

    元素 DQS-2 DQS-3 DQS-4
    本法(%) 化学法(%) 本法(%) 化学法(%) 本法(%) 化学法(%)
    Na2O 1.61 1.59 2.03 2.04 1.71 1.73
    MgO 5.65 5.58 0.60 0.52 0.078 0.070*
    Al2O3 19.63 19.48 27.89 27.99 29.92 29.77
    SiO2 40.79 40.65 39.57 39.69 52.99 52.74
    P2O5 0.21 0.19 0.009 0.011 0.13 0.12
    K2O 0.18 0.17 0.064 0.050 0.54 0.57
    CaO 7.47 7.38 0.57 0.49 1.19 1.10
    TiO2 0.47 0.45 0.18 0.18 0.010 0. 013*
    V2O5 0.033 0.034 - - - -
    Cr2O3 0.023 0.024 - - - -
    MnO 0.13 0.13 0.26 0.24 0.035 0.031
    TFe2O3 8.77 8.64 17.71 17.52 0.10 0.10
    注:标注“*”的数据表示该数据为高压密闭酸溶,ICP-OES法测定值;“-”表示低于检出限,没有提供测定值。
    下载: 导出CSV
  • [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. http://d.wanfangdata.com.cn/Periodical_dxqy201405028.aspx

    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. http://d.wanfangdata.com.cn/Periodical_dxqy201405028.aspx

    [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. http://www.oalib.com/paper/4763805

    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. http://www.oalib.com/paper/4763805

    [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

    [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.

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

    [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. https://pubs.geoscienceworld.org/msa/ammin/article-abstract/73/3-4/424/42164/ree-distributions-in-tourmaline-an-inaa-technique?redirectedFrom=fulltext

    [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

    [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. https://link.springer.com/article/10.1007/s10967-012-1954-0

    [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. http://www.ykcs.ac.cn/article/doi/10.15898/j.cnki.11-2131/td.201609220143

    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. http://www.ykcs.ac.cn/article/doi/10.15898/j.cnki.11-2131/td.201609220143

    [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

    [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

    [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. https://www.sciencedirect.com/science/article/pii/S1386142517303001

    [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. http://www.cnki.com.cn/Article/CJFDTotal-YJFX201507001.htm

    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. http://www.cnki.com.cn/Article/CJFDTotal-YJFX201507001.htm

    [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. http://www.rigaku.com/downloads/journal/RJ31-2/Rigaku%20Journal%2031-2_12-17.pdf

    [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. http://www.ykcs.ac.cn/article/id/ykcs_20090220

    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. http://www.ykcs.ac.cn/article/id/ykcs_20090220

    [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. http://d.wanfangdata.com.cn/Periodical_yjfx201309007.aspx

    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. http://d.wanfangdata.com.cn/Periodical_yjfx201309007.aspx

    [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

    [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. http://www.cnki.com.cn/Article/CJFDTOTAL-YHYJ201602007.htm

    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. http://www.cnki.com.cn/Article/CJFDTOTAL-YHYJ201602007.htm

  • 加载中

(7)

计量
  • 文章访问数:  4418
  • PDF下载数:  94
  • 施引文献:  0
出版历程
收稿日期:  2016-10-26
修回日期:  2017-04-30
录用日期:  2017-06-15

目录