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首页> 外文期刊>American Mineralogist >Influence of F content on the composition of Al-rich synthetic phlogopite: Part I. New information on structure and phase-formation from 29Si, 1H, and 19F MAS NMR spectroscopies
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Influence of F content on the composition of Al-rich synthetic phlogopite: Part I. New information on structure and phase-formation from 29Si, 1H, and 19F MAS NMR spectroscopies

机译:F含量对富Al合成金云母的组成的影响:第一部分。有关29Si,1H和19F MAS NMR光谱学的结构和相形成的新信息

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摘要

The influence of F content on the formation and stability of Al-rich phlogopite has been investigated. Samples with varying OH/F-ratios and nominal gel compositions of K(Mg3–xAlx)(Al1+xSi3–xO10)(OH)y(F)2–y (0.0 x 0.8 and 0.5 y 1.8) were studied using 29Si, 1H, and 19F MAS NMR spectroscopies, powder X-ray diffraction, electron-probe microanalysis, and scanning electron microscopy. The synthetic phlogopites were synthesized from sol-gels in cold-seal pressure vessels at 1073 K, 2 kbar. The main phase (phlogopite) and three other impurity phases [corundum (-Al2O3), kalsilite (KAlSiO4), and potassium aluminum hexafluoride (K3AlF6·0.5H2O)] were clearly identified by powder X-ray diffraction and electron-probe microanalysis. For phlogopite, the unit-cell parameters a0 and b0 decrease whereas c0 increases with increasing Al-content (x). The average crystal size of phlogopite is about 1–2 µm. The 29Si MAS NMR spectra show up to four resonances at approximately –91, –87, –83, and –80 ppm, which can be assigned as Q3(n Al) signals with n = 0–3. The ideal Si/IVAl ratio calculated from the initial composition is always lower than that derived experimentally. Hydroxyl-rich compositions indicate an increased Al-content in the tetrahedral sheets, suggesting a stabilizing effect on the formation of Al-rich phlogopite. These conclusions are supported by 1H and 19F MAS NMR spectra. The 1H MAS NMR spectra show a water signal at 4.7 ppm, a signal due to Mg2AlOH at 1.8 ppm, and a signal due to Mg3OH at 0.7 ppm. The 19F MAS NMR spectra exhibit a signal for Mg2AlF at –150 ppm, one due to AlF6 (K3AlF6·0.5H2O) at –157 ppm, and one for Mg3F at –174 ppm. Comparison of the 1H and 19F MAS NMR spectra for different Al- and F-contents reveals a non-statistical distribution of F- and OH-groups at the crystallographic sites in the octahedral sheets where F prefers sites coordinated by three Mg, and OH sites with Al in the next-nearest coordination sphere.
机译:研究了F含量对富铝金云母 金云母的形成和稳定性的影响。具有不同 OH / F比和标称凝胶组成为K(Mg 3-x Al x )(Al 1+ x Si 3-x O 10 )(OH) y (F) 2-y 使用 29 Si, 1 H和 研究了 (0.0 x 0.8和0.5 y 1.8) 19 F MAS NMR光谱学,粉末X射线衍射,电子探针 显微分析和扫描电子显微镜。合成的 phlogopites是在1073 K,2 kbar的冷密封压力容器中由溶胶-凝胶合成的。主相(金云母)和其他三个 杂质相[刚玉(-Al 2 O 3 ),钾铝石(KAlSiO 4 < / sub>), 和六氟化钾铝(K 3 AlF 6 ·0.5H 2 O)] <通过粉末X射线衍射和电子探针 微观分析可以清楚地识别出sup> 。对于金云母,单位晶格参数a 0 b 0 减小,而c 0 随Al-的增加而增加content (x)。金云母的平均晶体尺寸约为1-2 µm。 29 Si MAS NMR谱图显示在大约–91,–87,–83和–80 ppm处最多出现四个共振 。被分配为n = 0–3的Q 3 (n Al)信号。 根据初始成分计算出的理想Si / IV Al比 始终低于实验得出的值。富含羟基的 成分表明四面体 薄片中的铝含量增加,表明对富含 Al的金云母的形成具有稳定作用。这些结论得到 1 H和 19 F MAS NMR谱的支持。 1 H MAS NMR光谱显示水信号 为4.7 ppm,Mg 2 AlOH的信号为1.8 ppm,信号< sup> 归因于Mg 3 OH的含量为0.7 ppm。 19 F MAS NMR谱图显示–150 ppm时Mg 2 AlF的信号 ,这是由于AlF 6 (k 3 AlF 6 ·0.5H 2 O) ,浓度为–157 ppm,Mg < sub> 3 F在–174 ppm。不同Al和F含量的 1 H和 19 F MAS NMR谱的比较 揭示了一个非八面体薄片中 的晶体学位置的F-和OH-基的统计分布,其中F 首选由三个Mg配位的位点,OH配Al < / sup>在最近的协调领域。

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  • 来源
    《American Mineralogist》 |2003年第1期|00000047-00000053|共7页
  • 作者单位

    Institut für Mineralogie, Universit?t Hannover, Welfengarten 1, 30167 Hannover, Germany;

    Institut für Mineralogie, Universit?t Hannover, Welfengarten 1, 30167 Hannover, Germany;

    Institut für Mineralogie, Universit?t Hannover, Welfengarten 1, 30167 Hannover, Germany;

    The University of British Columbia, Department of Chemistry, 2036 Main Mall, Vancouver, B.C., V6T 1Z1, Canada;

    The University of British Columbia, Department of Earth and Ocean Sciences, 6339 Stores Road, Vancouver, B.C., V6T 1Z4, Canada;

    The University of British Columbia, Department of Earth and Ocean Sciences, 6339 Stores Road, Vancouver, B.C., V6T 1Z4, Canada;

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