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The role of SO42- surface distribution in arsenic removal by iron oxy-hydroxides

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Autore
Tresintsi, S.; Simeonidis, K.; Pliatsikas, N.; Vourlias, G.; Patsalas, P.; Mitrakas, M.
Data
2014
DOI
10.1016/j.jssc.2014.02.026
Soggetto
Sulfate
Iron oxy-hydroxides
Arsenic adsorption
XPS
FTIR
ION CHROMATOGRAPHY
SULFATE ADSORPTION
AQUEOUS-SOLUTIONS
GOETHITE
SORPTION
WATER
PRECIPITATION
INTERFACE
HEMATITE
SCHWERTMANNITE
Chemistry, Inorganic & Nuclear
Chemistry, Physical
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Abstract
This study investigates the contribution of chemisorbed SO42- in improving arsenic removal properties of iron oxy-hydroxides through an ion-exchange mechanism. An analytical methodology was developed for the accurate quantification of sulfate ion (SO42-) distribution onto the surface and structural compartments of iron oxy-hydroxides synthesized by FeSO4 precipitation. The procedure is based on the sequential determination of SO42- presence in the diffuse and Stern layers, and the structure of these materials as defined by the sulfate-rich environments during the reaction and the variation in acidity (pH 3-12). Physically sorbed SO42-, extracted in distilled water, and physically/chemically adsorbed ions on the oxy-hydroxide's surface leached by a 5 mM NaOH solution, were determined using ion chromatography. Total sulfate content was gravimetrically measured by precipitation as BaSO4. To validate the suggested method, results were verified by X-ray photoelectron and Fourier-transformed infrared spectroscopy. Results showed that low precipitation pH-values favor the incorporation of sulfate ions into the structure and the inner double layer, while under alkaline conditions ions shift to the diffuse layer. (C) 2014 Elsevier Inc. All rights reserved.
URI
http://hdl.handle.net/11615/33705
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