首页> 外文期刊>X-Ray Spectrometry: An International Journal >Glass beads/x-ray fluorescence analyses of 42 components in felsic rocks
【24h】

Glass beads/x-ray fluorescence analyses of 42 components in felsic rocks

机译:玻璃质珠/长石岩石中42种成分的X射线荧光分析

获取原文
获取原文并翻译 | 示例
           

摘要

Fused borate glass beads were used for the determination of 42 components (Na, Mg, Al, Si, P, K, Ca, Sc, Ti, V, Cr, Mn, Fe Co, Ni, Cu, Zn, Ga, As, Rb, Sr, Y, Zr, Nb, Sn, Cs, Ba, La, Ce, Pr, Nd, Sm, Gd, Dy, Er, Yb, Hf, Ta, W, Pb, Th, and U) in felsic rocks using x-ray fluorescence spectrometry (XRF). Low-dilution glass beads with 1:1 sample-to-flux ratios (called 1:1 glass beads) were prepared using the double-fusing method to measure Sc, Sn, Cs, Hf, Ta, and rare earth elements. Double-fusing, which uses two heating stages with intervening cooling to room temperature, was used to prepare homogeneous 1:1 glass beads. Pulverized rock samples of less than 20 gm modal diameter enabled us to prepare homogeneous 1:1, 1:2, and 1:10 glass beads. The glass bead thickness was set as constant because the fluorescent x-ray intensity of heavier elements, such as Rb, Sr, Y, and Zr, was influenced by thickness of 1:10 glass beads. Mutual interference of the nine analytical lines, V K alpha, Cr K alpha, Y K alpha, Zr K alpha, Nb K alpha, Ba L alpha, Ce L alpha, Er L alpha, and Yb L alpha, was corrected using the intensities of Ti K alpha, V K alpha, Rb K alpha, Sr K alpha, Y K alpha, Rb K alpha, Ba L alpha, Zr K alpha, and Ni K beta, corresponding to each overlap. Calibration curves of the 42 components showed good linearity (coefficient of determination, r = 0.991-1.000). The calibration ranges, indicating lower and upper limits of detection, were 1.6-58 to 0.03-7.6 mass ppm for the major elements (Na2O, MgO, Al2O3, SiO2, P2O5, K2O, CaO, TiO2, MnO, and Fe2O3) in 1:10 glass beads, 0.2-0.5 to 50-100 mass ppm for Rb, Sr, Y, and Zr in 1:10 glass beads, 0.3-6.0 to 20-230 mass ppm for minor elements (V, Cr, Co, Ni, Cu, Zn, Ga, As, Nb, Ba, W, Pb, Th, and U) in 1:2 glass beads, and 0.7-8.9 to 20-220 mass ppm for trace elements (Sc, Sn, Cs, Hf, Ta, and rare earth elements) in 1:1 glass beads. Using this method, we determined 42 components in two granites from Japan, weathered granite, obsidian, and rhyolite. Copyright (C) 2007 John Wiley & Sons, Ltd.
机译:熔融硼酸盐玻璃珠用于测定42种成分(Na,Mg,Al,Si,P,K,Ca,Sc,Ti,V,Cr,Mn,Fe Co,Ni,Cu,Zn,Ga,As, Rb,Sr,Y,Zr,Nb,Sn,Cs,Ba,La,Ce,Pr,Nd,Sm,Gd,Dy,Er,Yb,Hf,Ta,W,Pb,Th和U)使用X射线荧光光谱仪(XRF)。使用双熔法测量Sc,Sn,Cs,Hf,Ta和稀土元素,制备出具有1:1样品与助熔剂比率的低稀释玻璃珠(称为1:1玻璃珠)。使用两个加热阶段并在中间冷却至室温的双熔法制备均匀的1:1玻璃珠。模态直径小于20克的粉碎岩石样品使我们能够制备均质的1:1、1:2和1:10玻璃珠。玻璃珠的厚度设置为常数是因为较重元素(如Rb,Sr,Y和Zr)的荧光X射线强度受1:10玻璃珠的厚度影响。使用Ti的强度校正了VK alpha,Cr K alpha,YK alpha,Zr K alpha,Nb K alpha,Ba L alpha,Ce L alpha,Er L alpha和Yb L alpha这9条分析线的相互干扰。对应于每个重叠的K alpha,VK alpha,Rb K alpha,Sr K alpha,YK alpha,Rb K alpha,Ba L alpha,Zr K alpha和Ni K beta。 42种组分的校准曲线显示出良好的线性(测定系数,r = 0.991-1.000)。 1中主要元素(Na2O,MgO,Al2O3,SiO2,P2O5,K2O,CaO,TiO2,MnO和Fe2O3)的校准范围(指示检测下限和上限)为1.6-58至0.03-7.6质量ppm :10个玻璃珠,1:10玻璃珠中的Rb,Sr,Y和Zr为0.2-0.5至50-100质量ppm,微量元素(V,Cr,Co,Ni为0.3-6.0至20-230质量ppm ,Cu,Zn,Ga,As,Nb,Ba,W,Pb,Th和U)在1:2玻璃珠中,微量元素(Sc,Sn,Cs,Hf为0.7-8.9至20-220质量ppm ,钽和稀土元素)放入1:1的玻璃珠中。使用这种方法,我们确定了来自日本的两个花岗岩(风化花岗岩,黑曜石和流纹岩)中的42种成分。版权所有(C)2007 John Wiley&Sons,Ltd.

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号