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Stability constants for silicate adsorbed to ferrihydrite

Published online by Cambridge University Press:  09 July 2018

H. C. B. Hansen ,
T. P. Wetche ,
K. Raulund-Rasmussen  and
O. K. Borggaard
H. C. B. Hansen
Affiliation:
Chemistry Department, Royal Veterinary & Agricultural University, Thorvaldsensvej 40, DK-1871 Frdb. C., Copenhagen, Denmark
T. P. Wetche
Affiliation:
Chemistry Department, Royal Veterinary & Agricultural University, Thorvaldsensvej 40, DK-1871 Frdb. C., Copenhagen, Denmark
K. Raulund-Rasmussen
Affiliation:
Chemistry Department, Royal Veterinary & Agricultural University, Thorvaldsensvej 40, DK-1871 Frdb. C., Copenhagen, Denmark
O. K. Borggaard
Affiliation:
Chemistry Department, Royal Veterinary & Agricultural University, Thorvaldsensvej 40, DK-1871 Frdb. C., Copenhagen, Denmark
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Abstract

Intrinsic surface acidity constants (Kalintr, Ka2intr) and surface complexation constant for adsorption of orthosilicate onto synthetic ferrihydrite (Ksi for the complex ≡FeOSi(OH)3) have been determined from acid/base titrations in 0.001-0.1 M NaClO4 electrolytes and silicate adsorption experiments in 0.01 M NaNOi electrolyte (pH 3-6). The surface equilibrium constants were calculated according to the two-layer model by Dzombak ' Morel (1990). Near equilibrium between protons/hydroxyls in solution and the ferrihydrite surface was obtained within minutes while equilibration with silicate required days-weeks, both reactions probably being diffusion controlled. Applying the values for specific surface area and site densities for ferrihydrite used by Dzombak ' Morel (1990) (600 m2 g–1, 3.4 μmole m–2) the constants pKalintr = 6.93 ± 0.12, pKa2intr = 8.72 ± 0.17 and log Ksi = 3.62 were calculated by using the FITEQL optimization routine. Use of the specific surface area actually measured (269 m2 g-1) gave a poorer fit of the experimental data. Due to the slow adsorption of silicate and hence long shaking times, changes in the surface characteristics of the ferrihydrite seem to take place, probably a decrease in the concentration of surface sites. Adsorption isotherms calculated using the derived equilibrium constants showed that approximately twice the amount of silicate was adsorbed at pH 5 compared with pH 3.

Infrared spectroscopy of silica adsorbed to ferrihydrite showed Si-O stretching absorption maxima in the range 940-960 cm-1. The shift of the absorption maximum to higher wavenumbers with increasing amount of silicate adsorbed is probably due to an increase in the frequency of Si-O-Si bonds between orthosilicate adsorbed at adjacent sites. Small amounts of goethite were identified in the adsorption products.

Type
Research Article
Information
Clay Minerals , Volume 29 , Issue 3 , September 1994 , pp. 341 - 350
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

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