The Effect of Surface Modification by an Organosilane on the Electrochemical Properties of Kaolinite
- 1 April 1994
- journal article
- Published by Cambridge University Press (CUP) in Clays and Clay Minerals
- Vol. 42 (2), 123-136
- https://doi.org/10.1346/ccmn.1994.0420203
Abstract
The electrochemical properties of kaolinite before and after modification with chlorodimethyl-octadecylsilane have been studied by electrophoretic mobility, surface charge titration, and extrapolated yield stress measurements as a function of pH and ionic strength. A heteropolar model of kaolinite, which views the particles as having a pH-independent permanent negative charge on the basal planes and a pH-dependent charge on the edges, has been used to model the data. The zeta potential and surface charge titration experimental data have been used simultaneously to calculate acid and ion complexation equilibrium constants using a surface complex model of the oxide-solution interface. The experimental data were modeled following subtraction of the basal plane constant negative charge, describing only the edge electrical double layer properties. Extrapolated yield stress measurements along with the electrochemical data were used to determine the edge isoelectric points for both the unmodified and modified kaolinite and were found to occur at pH values of 5.25 and 6.75, respectively. Acidity and ion complexation constants were calculated for both sets of data before and after surface modification. The acidity constants, pKa1 = 5.0 and pKa2 = 6.0, calculated for unmodified kaolinite, correlate closely with acidity constants determined by oxide studies for acidic sites on alumina and silica, respectively, and were, therefore, assigned to pH-dependent specific chemical surface hydroxyl groups on the edges of kaolinite. The parameters calculated for the modified kaolinite indicate that the silane has reacted with these pH-dependent hydroxyl groups causing both a change in their acidity and a concomitant decrease in their ionization capacity. Infrared data show that the long chain hydrocarbon silane is held by strong bonding to the kaolinite surface as it remains attached after washing with cyclohexane, heating, and dispersion in an aqueous environment.This publication has 22 references indexed in Scilit:
- Adsorption of paraquat ions on clay minerals. Electrophoresis of clay particlesPublished by Springer Nature ,2007
- Rheology of Concentrated SuspensionsPublished by Springer Nature ,1990
- Exchange enthalpies of H+ and OH− adsorption on minerals with different characters of potential-determining ionsJournal of Colloid and Interface Science, 1988
- Surface ionization and complexation models: A comparison of methods for determining model parametersJournal of Colloid and Interface Science, 1987
- Kinetics and mechanism of dissolution of bayerite (γ-Al(OH)3) in HNO3-HF solutions at 298.2°KJournal of Colloid and Interface Science, 1984
- Silane Coupling AgentsPublished by Springer Nature ,1982
- Characterization of Aqueous Colloids by Their Electrical Double-Layer and Intrinsic Surface Chemical PropertiesPublished by Springer Nature ,1982
- A comparison of electrostatic models for the oxide/solution interfaceAdvances in Colloid and Interface Science, 1980
- Electrophoresis and zeta potential of kaoliniteJournal of Colloid and Interface Science, 1978
- Particle interactions in aqueous kaolinite suspensionsJournal of Colloid and Interface Science, 1977