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PREPARATION OF METAL OXIDE POWDERS USING ACTIVATED BALL MILLING

机译:活性球磨法制备金属氧化物粉末

摘要

Total phase transformation of hematite to magnetite was accomplished at room temperature by wet magnetomechanical activation of hematite. Low energy mechanical activation of the oxide surface is sufficient to effect the transformation. Oxygen bonds on a α-Fe2O3 oxide surface are apparently broken during the mechanical activation process and oxygen is released (removed) to the dispersing polar liquid. The oxygen pressure during the process as well as the nature of the dispering liquid have a critical influence on successful and fast phase transformation. Thus, all preparation performed in air, dry conditions or with nonpolar or saturated hydrocarbons (benzene, anthracene) show that the process of hematite reduction is non existent or very slow. Normal air pressure and/or application of hydrocarbons suppress the transformation. The effects of prolonged milling in air and vacuum on BaFe12O19 ionic crystal structure and particle morphology have been analysed. X-ray diffraction, scanning electron microscopy and thermal analysis experiments show, that for vacuum milled material, the ordered structure transforms progressively into a stable disordered nanocrystalline phase. For air milled samples, apart from a structural transformation, chemical decomposition was found. Application of heat treatment restores perfect Ba-ferrite crystal structure with the particle remaining in the submicron size range. With structural changes during annealing, the magnetic properties were altered. Radically different hysteresis behaviour was obtained for powders annealed at 1273 K. The value of volume magnetisation 4πMs = 335.4 - 347.2 kA/m is near the value for premilled ferrite powder (10 % lower), but measured coercivity value Hc = 393.9 - 445.6 kA/m was improved quite remarkably by a factor of 6 due to the fine crystalline grain structure.
机译:赤铁矿向磁铁矿的总相变在室温下通过赤铁矿的湿磁机械活化来完成。氧化物表面的低能机械活化足以实现该转变。在机械活化过程中,α-Fe2O3氧化物表面上的氧键显然被破坏,氧被释放(除去)到分散的极性液体中。在此过程中的氧气压力以及分散液的性质对成功和快速的相变具有至关重要的影响。因此,在空气,干燥条件下或与非极性或饱和烃类(苯,蒽)一起进行的所有制备均表明,赤铁矿还原过程不存在或非常缓慢。正常的气压和/或碳氢化合物的施加会抑制转化。分析了在空气和真空中长时间研磨对BaFe12O19离子晶体结构和颗粒形态的影响。 X射线衍射,扫描电子显微镜和热分析实验表明,对于真空研磨的材料,有序结构逐渐转变为稳定的无序纳米晶相。对于空气研磨的样品,除结构转变外,还发现化学分解。热处理的应用恢复了完美的钡铁氧体晶体结构,且颗粒保持在亚微米尺寸范围内。随着退火过程中结构的变化,磁性能发生了变化。对于在1273 K下退火的粉末,获得了截然不同的磁滞特性。体积磁化强度4πMs= 335.4-347.2 kA / m的值接近于预研磨的铁氧体粉末的值(低10%),但测得的矫顽力值Hc = 393.9-445.6 kA / m由于细晶粒结构而显着提高了6倍。

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