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Role of crystal structure in flotation separation of diaspore from kaolinite, pyrophyllite and illite

机译:晶体结构在水硬石浮选分离高岭石,叶蜡石和伊利石中的作用

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摘要

Wettability and electrokinetics of kaolinite, illite, pyrophyllite and diaspore were measured in the context of reverse flotation using cationic collectors. The results were interpreted by crystal structure analysis of the minerals. The point of zero charge (PZC) was calculated using crystallographic parameters of the minerals and compared well with the corresponding iso-electrical point (IEP) determined experimentally. The decreasing order of the measured IEP or calculated PZC from diaspore to kaolinite, illite and finally pyrophyllite correlated well with decreasing the number of broken Al-O bonds and the ratio of broken Al-O to Si-O bonds. The electrostatic interaction was identified as the main driving force for cationic collector adsorption on the minerals. Satisfactory separation of aluminosilicates from diaspore was achieved by reverse flotation.
机译:高岭石,伊利石,叶蜡石和水辉石的润湿性和电动势是在阳离子浮选法的反浮选条件下测量的。通过矿物的晶体结构分析来解释结果。使用矿物的晶体学参数计算零电荷点(PZC),并将其与实验确定的相应等电点(IEP)进行比较。从水硬石到高岭石,伊利石,最后到叶蜡石,测得的IEP或计算出的PZC的降序与减少的Al-O键数目和Al-O断裂键与Si-O键的比率相关。静电相互作用被确定为阳离子收集剂吸附在矿物上的主要驱动力。通过反向浮选可将铝硅酸盐与水铝石分离良好。

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