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首页> 外文期刊>Plasma Chemistry and Plasma Processing >Effect of Low Temperature Air Plasma Treatment on Wetting and Flow Properties of Kaolinite Powders
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Effect of Low Temperature Air Plasma Treatment on Wetting and Flow Properties of Kaolinite Powders

机译:低温空气等离子体处理对高岭石粉润湿和流动性能的影响

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It was found in this study that the air plasma treatment of particular kaolinite has led to the change of its wettability, which was reflected in the decreased values of water contact angles of wetting from 88.7° for virgin kaolinite to 86.3° for 30 min air plasma treated one. Plasma treated samples show higher average surface energies in the wide range of coverage regimes in comparison to the virgin samples as determined by inverse gas chromatography. Results of these measurements confirmed our assumption, that air plasma treatment activates surface energy of the crystal planes of the kaolinite as reflected in the broadened dispersive surface energy distribution after 10 min treatment time. However with prolonged 30 min treatment time the dispersive surface energy distribution profile was decreased. We assume, that the latter decrease reflects the distorsion of the crystal lattice of the kaolinite as confirmed by FTIR analysis as reflected in changes of Si–O–Si and Al2O–H characteristic absorption bands. Calculated dispersive surface free energy for 24 % surface coverage was increased from original 35 mJ/m2 to 40.3 and 40.8 mJ/m2 for 10 and 30 min treatment times. There were determined yield locus and flow function dependencies at different stress levels for virgin and different time plasma treated samples (flow index—ff c , effective angle of internal friction—φ e , unconfined yield strength—σ c ). It was found that by plasma treatment the character of the flow was shifting from region of very cohesive (ff c = 2.39) to the cohesive (ff c = 3.19). For untreated samples effective angle of internal friction was decreased with increasing applied consolidation stress, while for plasma treated kaolinite it was increased.
机译:在这项研究中发现,空气等离子处理特定的高岭石会导致其润湿性发生变化,这反映在水接触角的值从原始高岭石的88.7°降低到30分钟空气等离子的86.3°上。治疗一个。与通过逆气相色谱法测定的原始样品相比,经等离子体处理的样品在广泛的覆盖范围内显示出更高的平均表面能。这些测量结果证实了我们的假设,即空气等离子体处理会激活高岭石的晶面表面能,这一点反映在处理时间10分钟后变宽的分散表面能分布中。但是,随着处理时间延长30分钟,分散表面能分布曲线减小。我们认为,后者的减少反映了高岭石的晶格畸变,这是通过FTIR分析证实的,反映在Si–O–Si和Al2 O–H特征吸收带的变化中。在10和30分钟的处理时间内,计算出的24%表面覆盖率的分散表面自由能从原来的35 mJ / m2 增加到40.3和40.8 mJ / m2 。确定了原始和不同时间等离子体处理样品在不同应力水平下的屈服轨迹和流动函数依赖性(流动指数ff c ,有效内摩擦角φe ,无限制屈服强度σ c )。发现通过等离子体处理,流动的特性从非常内聚的区域(ff c = 2.39)转移到内聚的区域(ff c = 3.19)。对于未经处理的样品,有效的内摩擦角随施加的固结应力的增加而减小,而经等离子体处理的高岭石的内角则增大。

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