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Spectral induced polarization of Na-montmorillonite dispersions

Leroy, Philippe (author)
Uppsala universitet,Luft-, vatten- och landskapslära,French Geol Survey, BRGM, F-45060 Orleans, France
Weigand, Maximilian (author)
Univ Bonn, Steinmann Inst, Dept Geophys, D-53115 Bonn, Germany.
Meriguet, Guillaume (author)
Pierre & Marie Curie Univ, PHENIX, CNRS, UMR 8234, F-75252 Paris, France.
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Zimmermann, Egon (author)
Forschungszentrum Julich, Cent Inst Engn Elect & Analyt, Elect Syst, ZEA 2, D-52425 Julich, Germany.
Tournassat, Christophe (author)
Univ Orleans, CNRS INSU BRGM, UMR 7327, Inst Sci Terre Orleans, F-45071 Orleans, France.
Fagerlund, Fritjof, 1974- (author)
Uppsala universitet,Luft-, vatten- och landskapslära
Kemna, Andreas (author)
Univ Bonn, Steinmann Inst, Dept Geophys, D-53115 Bonn, Germany.
Huisman, Johan Alexander (author)
Forschungszentrum Julich, Inst Bio & Geosci, IBG 3, Agrosphere Inst, D-52425 Julich, Germany.
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 (creator_code:org_t)
ACADEMIC PRESS INC ELSEVIER SCIENCE, 2017
2017
English.
In: Journal of Colloid and Interface Science. - : ACADEMIC PRESS INC ELSEVIER SCIENCE. - 0021-9797 .- 1095-7103. ; 505, s. 1093-1110
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Montmorillonite (Mt) clays have a high specific surface area and surface charge, which confer them remarkable adsorption properties. Nevertheless, their electrochemical and aggregation behavior are not completely elucidated because of the complexity of their microstructural and interfacial properties. In this work, the conductive and dispersive properties of Na-Mt suspensions of weight fractions 0.5-5.2% were investigated for the first time using the spectral induced polarization method. A four-electrode system was used to reduce errors introduced by electrode polarization and contact resistances. Complex conductivity spectra in the low-frequency range of 0.1 Hz to 45 kHz were successfully described using a triple layer model of the basal surface of Mt and a complex conductivity model that considers conduction of the diffuse layer and polarization of the Stern layer. Aggregate size distributions were inferred from inverted relaxation time distributions. We found that the negative and permanent surface charge of the basal plane of Na-Mt controls its quadrature (imaginary) conductivity, which is not very sensitive to pH and salinity (NaCI) in the 100 Hz to 45 kHz frequency range. For lower frequencies, the sudden increase of the quadrature conductivity at the highest salinities was explained by considering coagulation of Na-Mt particles.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Keyword

Na-montmorillonite
Dispersions
Spectral induced polarization
Conductivity
Dielectric permittivity
Basal plane
Surface charge
Stern layer
Diffuse layer

Publication and Content Type

ref (subject category)
art (subject category)

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