2014
DOI: 10.1016/j.mineng.2013.06.004
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A preliminary rheological classification of phyllosilicate group minerals

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Cited by 91 publications
(53 citation statements)
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“…The p.z.c. values of these minerals have previously been measured at pH 2.3 for quartz and pH 6.8 for illite [15]. Therefore, any elevation in the p.z.c value due to edge sites could be depressed by these impurities, resulting in a lower measured value.…”
Section: Accepted M Manuscriptmentioning
confidence: 96%
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“…The p.z.c. values of these minerals have previously been measured at pH 2.3 for quartz and pH 6.8 for illite [15]. Therefore, any elevation in the p.z.c value due to edge sites could be depressed by these impurities, resulting in a lower measured value.…”
Section: Accepted M Manuscriptmentioning
confidence: 96%
“…The impurities comprised mainly of quartz and illite. It has previously been shown that these minerals do not affect the suspension rheology [14,15]. While the colloidal behaviour can still be assumed to be largely due to the bulk mineralogy i.e.…”
Section: Accepted Manuscriptmentioning
confidence: 99%
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“…The basal planes displaying an inert siloxane structure are commonly charged negative charge [41][42][43][44][45][46]. While the edge planes are consisting of alternating layers of tetrahedral silicates and octahedral aluminum oxy-hydroxides.…”
Section: Discussionmentioning
confidence: 99%
“…These forces in clay suspensions have been reviewed by McBride and Baveye [55]. The more recent possibility to add to these forces came from the observations [7,56] of higher surface concentrations of step (defect) sites on low-crystallinity…”
Section: Particle Size Effect and Surface Force Considerationsmentioning
confidence: 99%