Journal of Soil Science · 1972 · 682 citations · 22 references
Natural SciencesChemistryMaterials SciencePhysical ChemistrySurface ChemistrySurface ScienceAdsorption At InterfacesIon ExchangeMineral Surface ChemistrySurface AdsorptionSurface ReactivityAdsorption EquilibriaAdsorption Of FluorideAnion AdsorptionIon AdsorptionIonic StrengthIrreversibilityReversibilitySpecific Ion Adsorption
Summary The relationship between adsorption and pH, termed the adsorption envelope, varies with the p K a, of the conjugate acid of the anion, for several adsorbents in presence of an excess of specifically adsorbed anions. At pH values where the acid is fully dissociated, specific adsorption occurs only to the extent of the positive charge of the surface and little specific adsorption is found at pH values more alkaline than the zero point of charge (zpc). With incompletely dissociated acids, anion adsorption can also take place at pH values more alkaline than the zpc providing the pH is somewhere near a p K a value of the acid, where the energy required to abstract a proton from the acid is at a minimum. The proton is required for the removal of a surface OH which provides a site for the anion. Specific anion adsorption (i) from a fully dissociated acid can reduce the positive charge of the surface to zero and (ii) from a weak acid can make even a negative surface more negative. Thus specific adsorption shifts the zpc to more acid values. The relationship between anion adsorption and OH release is not necessarily simple. The ideas proposed for anion adsorption have implications for cation adsorption and incorporation in an oxide surface.
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W.J. Orville-Thomas · Journal of Molecular Structure · 1973 · 6.8K citations
THE ZERO POINT OF CHARGE OF OXIDES<sup>1</sup>
G.A. Parks, P.L. De Bruyn · The Journal of Physical Chemistry · 1962 · 802 citations
F. J. Hingston, Roger Atkinson, A. M. Posner et al. · Nature · 1967 · 462 citations
Frederick C. Nachod · Journal of the American Chemical Society · 1965 · 357 citations