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Characterisation of kaolinite colloidal and flow behaviour via crystallinity measurements

机译:通过结晶度测量表征高岭石胶体和流动行为

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摘要

This study evaluates the possibility of predicting colloidal and flow behaviour of kaolinite suspensions by measuring kaolinite crystallinity. The Hinckley index of different samples was calculated from XRD spectra as an indicator of the crystallinity. Kaolinite samples with a high Hinckley index showed a defined platy morphology with smooth surfaces of low surface area, whilst progressively roughened basal planes with prevalent broken edges were observed in kaolinite samples of lower Hinckley indices. Despite similarity in the elemental composition, the kaolinite samples present different surface charge properties, likely due to variations in exposed pH dependent edge sites. Poorly crystallised kaolinite samples were characterised by higher yield stresses and viscosities. This study highlights the importance of crystallinity characterisation towards predicting colloidal behaviour and flow characteristics of kaolinite suspensions.
机译:这项研究评估通过测量高岭石结晶度预测高岭石悬浮液的胶体和流动行为的可能性。由XRD光谱计算出不同样品的欣克利指数作为结晶度的指标。具有高欣克利指数的高岭石样品显示出定义的板状形态,具有低表面积的光滑表面,而在较低欣克利指数的高岭石样品中观察到逐渐粗糙的基面,且边缘普遍断裂。尽管元素组成相似,但高岭石样品仍具有不同的表面电荷性质,这可能是由于暴露的pH依赖性边缘位点的变化所致。结晶不良的高岭石样品的特征在于较高的屈服应力和粘度。这项研究强调了结晶度表征对于预测高岭石悬浮液的胶体行为和流动特性的重要性。

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