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Influence of mechanical activation on DC conductivity of kaolin

机译:机械活化对高岭土直流电导率的影响

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摘要

In this study, the effect of dry milling of kaolin (92 mass% of kaolinite) on its physical properties and microstructure development during firing was investigated using thermal analyses, X-ray diffraction, scanning electron microscopy, and DC conductivity measurements. X-ray diffraction showed a decrease in the intensity of reflections of kaolinite with rising milling time. Moreover, formation of agglomerates from kaolinite particles was observed. A longer milling time led to a lower dehydroxylation temperature and contributed to a more substantial overall contraction of samples. After dehydroxylation, the relative bulk density increased with an increasing milling time. Below the temperature 450 degrees C (start of dehydroxylation), the highest values of the DC conductivity of raw samples were observed for the longest milling times. The main charge carriers are the H+ and OH- ions, originated from dissociation of the adsorbed water and from the coordinated water that was formed during mechanical dehydroxylation of kaolinite, complemented with alkali ions Na+ and K+ which are present as impurities in kaolin. The presence of coordinated water was proven by increasing values of the DC conductivity and by decreasing values of conduction activation energy from 1.73 eV to 0.85 eV with increasing milling time. A similar trend of conduction activation energy was observed in the temperature range 650-750 degrees C, where the values of conduction activation energy changed from 0.79 eV to 0.52 eV with increasing milling time. After dehydroxylation (above 750 degrees C), the DC conductivity of raw samples slightly decreased with increasing milling time.
机译:在这项研究中,使用热分析,X射线衍射,扫描电子显微镜和直流电导率测量研究了干磨高岭土(92质量%的高岭石)对其焙烧过程中物理性能和微观结构的影响。 X射线衍射显示,随着研磨时间的增加,高岭石的反射强度降低。此外,观察到由高岭石颗粒形成附聚物。较长的研磨时间导致较低的脱羟基温度,并导致样品的整体收缩更大。脱羟基后,相对松密度随着研磨时间的增加而增加。低于温度450摄氏度(开始脱羟基),在最长的研磨时间内观察到了原始样品的直流电导率的最大值。主要的电荷载体是H +和OH-离子,它们源自被吸附的水的分解以及高岭石机械脱羟基过程中形成的配位水,并补充了作为杂质存在于高岭土中的碱金属离子Na +和K +。通过增加直流电导率的值以及随着研磨时间的增加将传导活化能的值从1.73 eV降低到0.85 eV,证明了配位水的存在。在650-750摄氏度的温度范围内观察到了类似的传导活化能趋势,其中随着研磨时间的增加,传导活化能的值从0.79 eV变为0.52 eV。脱羟基后(高于750摄氏度),原始样品的直流电导率随研磨时间的增加而略有下降。

著录项

  • 来源
    《Applied clay science》 |2018年第3期|36-42|共7页
  • 作者单位

    Constantine Philosopher Univ, Dept Phys, Nitra 94974, Slovakia;

    Constantine Philosopher Univ, Dept Phys, Nitra 94974, Slovakia;

    Constantine Philosopher Univ, Dept Phys, Nitra 94974, Slovakia;

    Constantine Philosopher Univ, Dept Phys, Nitra 94974, Slovakia;

    Charles Univ Prague, Fac Math & Phys, Ke Karlovu 3, Prague 12116, Czech Republic;

    Czech Tech Univ, Dept Mat Engn & Chem, Thakurova 7, Prague 16629, Czech Republic;

    Constantine Philosopher Univ, Dept Phys, Nitra 94974, Slovakia;

    Charles Univ Prague, Fac Math & Phys, Ke Karlovu 3, Prague 12116, Czech Republic;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Kaolin; Mechanical activation; DC conductivity;

    机译:高岭土;机械活化;直流电导率;

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