Dielectric properties of iron-bearing trioctahedral phyllosilicates

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Autoren

  • C. H. Rüscher
  • S. Gall

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OriginalspracheEnglisch
Seiten (von - bis)365-373
Seitenumfang9
FachzeitschriftPhysics and chemistry of minerals
Jahrgang24
Ausgabenummer5
PublikationsstatusVeröffentlicht - Juli 1997

Abstract

Measurements of the real part of conductivity (σ′) and dielectric function (ε′) were performed on large crystal flakes of biotite (Moen) and vermiculite (Benahavis), at variable frequencies (0.1 to 1000 kHz) and as a function of temperature (300 K<T<900 K). By heating, cooling and repeated heating experiments under inert atmospheric conditions effects involving water (H2O) diffusion and electrical transport were separated. The effect of dehydration dominates the functional dependence of ε′ T at frequencies below about 100 kHz, within the first heating run. Six dehydration steps for vermiculite Benahavis and two broad features for biotite Moen are observed, the water being transported effectively only in the interlayers. Electrical transport occurs along Fe paths within the octahedral layers and can be described by σ′=σdc + A · ws. Values of s are between 0.45 and 0.8. σdc shows a temperature dependence according to exp(-Ea(T)/kT) with Ea(T) between 0.3 and 0.6 eV. Ea is suggested to be composed of a polaron plus disorder contribution.

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Dielectric properties of iron-bearing trioctahedral phyllosilicates. / Rüscher, C. H.; Gall, S.
in: Physics and chemistry of minerals, Jahrgang 24, Nr. 5, 07.1997, S. 365-373.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Rüscher CH, Gall S. Dielectric properties of iron-bearing trioctahedral phyllosilicates. Physics and chemistry of minerals. 1997 Jul;24(5):365-373. doi: 10.1007/s002690050050
Rüscher, C. H. ; Gall, S. / Dielectric properties of iron-bearing trioctahedral phyllosilicates. in: Physics and chemistry of minerals. 1997 ; Jahrgang 24, Nr. 5. S. 365-373.
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