Cation intersite distributions in iron-bearing minerals via electrical conductivity/seebeck effect

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

The equilibrium high temperature cation intersite distributions in iron-bearing minerals which exhibit small polaron "hopping" conduction can be determined by a technique which combines electrical conductivity and Seebeck effect. The procedure is demonstrated for ferrospinels (Fe3O4) - FeAl2O4 and Fe3O4 - CoFe2O4) and applied to the olivine Fe2SiO4 - Mg2SiO4 system.

Original languageEnglish
Pages (from-to)156-162
Number of pages7
JournalPhysics and Chemistry of Minerals
Volume14
Issue number2
DOIs
Publication statusPublished - Feb 1987

Fingerprint

Bearings (structural)
Seebeck effect
Gene Conversion
Olivine
electrical conductivity
Minerals
Cations
olivine
Iron
cation
Positive ions
iron
mineral
Temperature
Electric Conductivity
forsterite
cobalt ferrite
effect
distribution

ASJC Scopus subject areas

  • Materials Science(all)
  • Geochemistry and Petrology
  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

Cite this

Cation intersite distributions in iron-bearing minerals via electrical conductivity/seebeck effect. / Mason, Thomas O.

In: Physics and Chemistry of Minerals, Vol. 14, No. 2, 02.1987, p. 156-162.

Research output: Contribution to journalArticle

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