Electron microprobe technique for the determination of iron oxidation state in silicate glasses

被引:29
|
作者
Zhang, Chao [1 ]
Almeev, Renat R. [1 ]
Hughes, Ery C. [2 ]
Borisov, Alexander A. [3 ]
Wolff, Eric P. [1 ]
Hoefer, Heidi E. [4 ]
Botcharnikov, Roman E. [5 ]
Koepke, Juergen [1 ]
机构
[1] Leibniz Univ Hannover, Inst Mineral, Callinstr 3, D-30167 Hannover, Germany
[2] Univ Bristol, Sch Earth Sci, Bristol BS8 1RJ, Avon, England
[3] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Staromonetny 35, Moscow 109017, Russia
[4] Goethe Univ Frankfurt, Inst Geowissensch Mineral, Altenhoferallee 1, D-60438 Frankfurt, Germany
[5] Johannes Gutenberg Univ Mainz, Inst Geowissensch, J-J Becher Weg 21, D-55128 Mainz, Germany
关键词
Microprobe; ferric-ferrous ratio; silicate glasses; redox state; flank method; pillow glasses; PROBE MICROANALYSIS; OXYGEN FUGACITY; MORB GLASSES; FE; MINERALS; FE3+/SIGMA-FE; RATIOS; ENERGY; WATER; CALIBRATION;
D O I
10.2138/am-2018-6437
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a new calibration for the determination of the iron oxidation state in silicate glasses by electron probe microanalysis (EPMA) with the "flank method." This method is based on the changes in both intensity and wavelength of the FeL alpha and FeL beta X-ray emission lines with iron oxidation state. The flank method utilizes the maximum difference for the FeL alpha and FeL beta spectra observed at the peak flanks between different standard materials, which quantitatively correlates with the Fe2+ content. Provided that this correlation is calibrated on reference materials, the Fe2+/Sigma Fe ratio can be determined for samples with known total Fe content. Two synthetic Fe-rich ferric and ferrous garnet end-members, i.e., andradite and almandine, were used to identify the FeL alpha and FeL beta flank method measuring positions that were then applied to the measurement of a variety of silicate glasses with known Fe2+/Sigma Fe ratio (ranging from 0.2 to 1.0). The measured intensity ratio of FeL beta over FeL alpha at these flank positions (L beta/L alpha) is a linear function of the Fe2+ content (in wt%). A single linear trend can be established for both garnets and silicate glasses with 4-18 wt% FeOT (total iron expressed as FeO). In glasses with up to 18 wt% FeOT and 15 wt% TiO2, no systematic compositional (matrix) effects were observed. A possible influence of Ti on the Fe2+ determination has only been observed in one high-Ti glass with similar to 25 wt% TiO2, a content that is not typical for natural terrestrial silicate melts. The accuracy of the Fe2+/Sigma Fe determination, which depends on both the Fe2+ content determined with the flank method and on the total Fe content, is estimated to be within +/- 0.1 for silicate glasses with FeOT > 5 wt% and within +/- 0.3 for silicate glasses with low FeOT <= 5 wt%. The application of the flank method on silicate glasses requires minimization of the EPMA beam damage that can be successfully achieved by continuous movement of the sample stage under the electron beam during analysis, e.g., with a speed of 2 mu m/s.
引用
收藏
页码:1445 / 1454
页数:10
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