2000
DOI: 10.1016/s0301-7516(99)00041-1
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Surface chemistry–rheology relationships in concentrated mineral suspensions

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Cited by 322 publications
(173 citation statements)
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“…However, given the pH-dependence and anisotropy of surface charge for the irregular-shaped clay minerals, as well as their interactions with a myriad of dissolved species in typical industrial process water, additional non-DLVO interactions and complex dispersion stability behaviours can be expected and have indeed been reported Johnson, et al, 2000). Hydration and steric interactions stemming from adsorbed layers of water and macromolecules increase the mutual repulsion between suspended particles, while surfactantmodified or naturally hydrophobic particle surfaces experience an additional attraction to surfaces of similar nature -hydrophobic force (Israelachvili, 2011).…”
Section: Size Classificationmentioning
confidence: 99%
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“…However, given the pH-dependence and anisotropy of surface charge for the irregular-shaped clay minerals, as well as their interactions with a myriad of dissolved species in typical industrial process water, additional non-DLVO interactions and complex dispersion stability behaviours can be expected and have indeed been reported Johnson, et al, 2000). Hydration and steric interactions stemming from adsorbed layers of water and macromolecules increase the mutual repulsion between suspended particles, while surfactantmodified or naturally hydrophobic particle surfaces experience an additional attraction to surfaces of similar nature -hydrophobic force (Israelachvili, 2011).…”
Section: Size Classificationmentioning
confidence: 99%
“…Consequently, the solids aggregate at larger separation distances where the secondary interaction energy minimum occurs to form loose and porous aggregates. For clays, a "card house" structure is often observed at intermediate pH and for low aspect ratio clays, where the dominant inter-particle orientation consists of basal plane-edge surface interaction due to anisotropic surface charge characteristics of basal planes and edge surfaces, as shown in Figure 3 (Johnson, et al, 2000;Gupta, et al, 2011;Yan, et al, 2013). At high pH, the charge repulsion between the negatively charged basal plane and edge surface is sufficient to stabilize the particles in the suspension.…”
Section: Slurry Rheologymentioning
confidence: 99%
“…This renders the edge charge more significant. The changes in particle alignment as a function of pH are discussed in more detail by several researchers [1,2,7].…”
Section: Accepted M Manuscriptmentioning
confidence: 99%
“…Therefore, at pH conditions well above the edge i.e.p, the system should become dispersed, due to the repulsion between edge and basal face sites. On this basis, it is generally assumed that all kaolinite suspensions will predominantly comprise a combination of EE and dispersed structures at pH 9 [7]. Such suspensions would be characterised by low yield stresses and viscosities.…”
Section: Rheological Characterisationmentioning
confidence: 99%
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