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Structural change of alkali feldspar by ball milling

机译:球磨制碱长石的结构变化

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摘要

The structural changes and amorphization of alkali feldspar by ball milling were investigated using X-ray diffraction (XRD), Fourier-transform infrared (FTIR) spectroscopy, Raman spectroscopy, scanning electron microscopy (SEM), thermal analysis, particle size analysis, and specific surface area measurements. The Or_(77)Ab_(23) alkali feldspar crystal has an Ab-rich lamella texture in Or-rich host crystals. The mean particle size decreased from ~67 μm to almost 3 μm after 50 h of ball milling. After 600 h of ball milling, the apparent mean particle size calculated from the observed particle size distribution increased prominently because of the agglomeration of small particles. It reached ~ 38 μm after 1200 h of ball milling. While the density variation was not consistent with that of the particle size, it was consistent with that of the crystallinity estimated from X-ray diffraction data. The FTIR and Raman spectra indicated breaking of the Si-O-Si or Al-O-Si bonds and the formation of defects and distortion of the TO_4 (T = Si or Al) tetrahedra as a result of the milling. An increase in the intensity of luminescence with milling supported these results. XRD analysis revealed the sample that was ball milled for 1200-h was amorphous. However, the structure and properties of this amorphous phase were different from those of fused feldspar glass and had weak crystalline features. These amorphous materials were similar to those in the fault zone that were formed naturally and experimentally without melting. The Si-OH (or Al-OH) shoulders v = 890 cm~(-1)) in the FTIR spectra were formed by the chemical reaction between the broken Si-O-Si (or Al-O-Si) bonds and atmospheric water surrounding the 300-h milled samples. Because of this reaction, the surface and interior structure of the milled particles depended on the agglomeration and formation of defects formation resulting from the long milling time. XRD results of the milled samples indicated that grains with a larger amount of Ab-rich lamella structures were downsized more rapidly than the Or-rich host.
机译:使用X射线衍射(XRD),傅里叶变换红外(FTIR)光谱,拉曼光谱,扫描电子显微镜(SEM),热分析,粒度分析和比色法研究了碱长石球磨的结构变化和非晶化表面积测量。 Or_(77)Ab_(23)碱性长石晶体在富含Or的主体晶体中具有富含Ab的薄片质地。球磨50 h后,平均粒径从〜67μm减小到近3μm。球磨600小时后,由于小颗粒的团聚,从观察到的粒径分布计算出的表观平均粒径显着增加。球磨1200h后达到〜38μm。尽管密度变化与粒度的变化不一致,但是其与根据X射线衍射数据估计的结晶度的变化一致。 FTIR和拉曼光谱表明,由于研磨,Si-O-Si或Al-O-Si键断裂,形成缺陷和TO_4(T = Si或Al)四面体的畸变。随着研磨的发光强度的增加支持了这些结果。 XRD分析表明,球磨1200小时的样品是无定形的。但是,该非晶相的结构和性质与熔融长石玻璃的结构和性质不同,并且具有弱的结晶特征。这些无定形材料类似于在断层带中的天然材料,并且在实验中没有熔化而形成。 FTIR光谱中的Si-OH(或Al-OH)肩v = 890 cm〜(-1))是由断裂的Si-O-Si(或Al-O-Si)键与大气之间的化学反应形成的300小时研磨样品周围的水。由于该反应,研磨颗粒的表面和内部结构取决于团聚以及由于长时间研磨而形成的缺陷形成。研磨样品的XRD结果表明,具有大量富含Ab的薄层结构的晶粒比富含Or的基质更快地减小了尺寸。

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  • 作者单位

    Department of Earth Science, Graduate School of Science and Technology, Kanazawa University, Kanazawa 920-1192, Japan;

    Department of Earth Science, Graduate School of Science and Technology, Kanazawa University, Kanazawa 920-1192, Japan;

    Department of Earth Science, Graduate School of Science and Technology, Kanazawa University, Kanazawa 920-1192, Japan;

    Department of Earth Science, Graduate School of Science and Technology, Kanazawa University, Kanazawa 920-1192, Japan;

    Department of Earth Science, Graduate School of Science and Technology, Kanazawa University, Kanazawa 920-1192, Japan;

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  • 正文语种 eng
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  • 关键词

    Alkali feldspar; Lamella; Ball-milling; Structural change; Amorphization;

    机译:碱土长石;薄片;球磨;结构变化;非晶化;

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