Electrical conductivity of majorite garnet and its implications for electrical structure in the mantle transition zone

Takashi Yoshino, Masayuki Nishi, Takuya Matsuzaki, Daisuke Yamazaki, Tomoo Katsura

Research output: Contribution to journalArticle

45 Citations (Scopus)

Abstract

Electrical conductivities of majorite garnet with compositions of pyrolite minus olivine (pyrolite majorite) and mid-ocean ridge basalt (MORB majorite) were measured under physical conditions of the mantle transition zone (18 and 23 GPa and temperatures up to 2000 K) in a Kawai-type multi-anvil apparatus. The samples with MORB composition are mainly composed of majorite, which has higher Fe and Al contents, and contain a small amount of stishovite. The conductivity of the MORB majorite is more than twice higher than those of the pyrolite majorite at the same temperature. The activation energies of these majorites are both 1.4 eV at temperature of 1000-1600 K suggesting that the dominant mechanism of charge transportation is Fe2+-Fe3+ hopping (small polaron) conduction. At higher temperatures (>1600 K), corresponding to temperature conditions of the transition zone, conduction mechanism of the pyrolite majorite would change from small polaron to ionic conduction. The pyrolite majorite has only slightly higher and lower conductivity than dry wadsleyite and ringwoodite, respectively, and will not largely change the conductivity-depth profile predicted for the dry mantle transition zone. The laboratory-based conductivity profile of the mantle transition zone with pyrolitic composition can explain well the current semi-global conductivity-depth profile obtained from electromagnetic study beneath Pacific. On the other hand, the garnetite originating from the oceanic crust has remarkably higher conductivity than the surrounding mantle because the conductivity of MORB majorite is significantly higher than those of wadsleyite and ringwoodite. Conductivity values of MORB majorite agree with those of the stagnant slab beneath the northeastern China.

Original languageEnglish
Pages (from-to)193-200
Number of pages8
JournalPhysics of the Earth and Planetary Interiors
Volume170
Issue number3-4
DOIs
Publication statusPublished - Nov 2008

Fingerprint

majorite
garnets
transition zone
electrical conductivity
garnet
Earth mantle
mantle
pyrolite
conductivity
electrical resistivity
mid-ocean ridge basalt
wadsleyite
ringwoodite
conduction
profiles
stishovite
low conductivity
temperature
mid-ocean ridges
anvils

Keywords

  • Electrical conductivity
  • Majorite
  • Mantle transition zone
  • MORB
  • Pyrolite

ASJC Scopus subject areas

  • Geophysics
  • Space and Planetary Science
  • Physics and Astronomy (miscellaneous)
  • Astronomy and Astrophysics

Cite this

Electrical conductivity of majorite garnet and its implications for electrical structure in the mantle transition zone. / Yoshino, Takashi; Nishi, Masayuki; Matsuzaki, Takuya; Yamazaki, Daisuke; Katsura, Tomoo.

In: Physics of the Earth and Planetary Interiors, Vol. 170, No. 3-4, 11.2008, p. 193-200.

Research output: Contribution to journalArticle

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