2015
DOI: 10.1016/j.colsurfa.2015.05.043
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Effect of Ca2+, Mg2+ and SO42− ions on the zeta potential of calcite and dolomite particles aged with stearic acid

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Cited by 114 publications
(121 citation statements)
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“…It can be speculated that the adsorption of Ca 2+ or Mg 2+ on the apatite surface can increase the active sites which react with the carboxylate ion of fatty acid soap, contributing to the improvement of apatite floatability. The high recovery of dolomite was mainly attributed to the relatively high concentration of cations in the surface lattice [24], thus a low concentration of Ca 2+ and Mg 2+ exhibited a negligible influence on the flotation performance of dolomite. However, in the case of high concentration, the extra divalent metal ions in the bulk would react with fatty acid soap, reducing the amount available for dolomite collection [12].…”
Section: Hydrolysis Equilibria Of Metal Ionsmentioning
confidence: 98%
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“…It can be speculated that the adsorption of Ca 2+ or Mg 2+ on the apatite surface can increase the active sites which react with the carboxylate ion of fatty acid soap, contributing to the improvement of apatite floatability. The high recovery of dolomite was mainly attributed to the relatively high concentration of cations in the surface lattice [24], thus a low concentration of Ca 2+ and Mg 2+ exhibited a negligible influence on the flotation performance of dolomite. However, in the case of high concentration, the extra divalent metal ions in the bulk would react with fatty acid soap, reducing the amount available for dolomite collection [12].…”
Section: Hydrolysis Equilibria Of Metal Ionsmentioning
confidence: 98%
“…Hence, the effect of calcium ions on the zeta potential of minerals was studied. Previous studies were focused separately on the zeta potential measurements of apatite [26,27], dolomite [24,28], and quartz [29] in the presence of calcium ions. In fact, the zeta potentials varied due to different ionic strength, experimental apparatus, sample preparation process, etc.…”
Section: Zeta Potentials Of Pure Minerals In the Presence Of Calcium mentioning
confidence: 99%
“…Cicerone et al, 1992, Vdovic, 2001, the importance of controlling CO2 partial pressure (pCO2) in open or closed-system experiments (Thompson and Pownall, 1989;Heberling et al, 2011), the impact of wetting state in the presence of NAPLs (e.g. Jackson and Vinogradov, 2012;Kasha et al, 2015), and the effect of PDI concentration (Pierre et al, 1990;Zhang and Austad, 2006;Strand et al, 2006;Alotaibi et al, 2011;Chen et al, 2014;Alotaibi and Yousef, 2015;Mahani et al, 2015a,b). However, few report measurements of zeta potential in carbonates at conditions relevant to natural subsurface systems.…”
Section: Introductionmentioning
confidence: 99%
“…The Zeta potentials of apatite, dolomite, and quartz decrease with the pH increasing among the tested pH range. Some literatures report that isoelectric point (IEP) value of apatite from different deposits changes from 2.0 to 8.0, and the dolomite is around 3.0-6.0, but they can shift in the presence of electrolyte (Yu et al, 1985;Merma et al, 2013;Kasha et al, 2015). Therefore, isoelectric points of apatite and dolomite in 10 mM KCl solutions are observed, but no isoelectric points of quartz are determined around the tested pH range from 3.1 to 10.2.…”
Section: Zeta Potentials Of Apatite Dolomite Quartzmentioning
confidence: 99%