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Iron-silica interaction at extreme conditions and the electrically conducting layer at the base of Earth's mantle

Dubrovinsky, L. (author)
Bayerisches Geoinstitut, Universität Bayreuth
Dubrovinskaia, N. (author)
Bayerisches Geoinstitut, Universität Bayreuth
Langenhorst, F. (author)
Bayerisches Geoinstitut, Universität Bayreuth
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Dobson, D. (author)
Bayerisches Geoinstitut, Universität Bayreuth
Rubie, D. (author)
Bayerisches Geoinstitut, Universität Bayreuth
Gessgmann, C. (author)
Max-Planck-Institut für Chemie, Mainz
Abrikosov, I. A. (author)
Condensed Matter Theory Group, Department of Physics, Uppsala University
Johansson, Börje (author)
KTH,Materialvetenskap
Baykov, Vitaly (author)
KTH,Materialvetenskap
Vitos, Levente (author)
KTH,Materialvetenskap
Le Bihan, T. (author)
European Synchrotron Radiation Facility, Grenoble
Crichton, W. A. (author)
European Synchrotron Radiation Facility, Grenoble
Dmitriev, V. (author)
Swiss-Norwegian Beam Lines at ESRF, Grenoble
Weber, H. P. (author)
Swiss-Norwegian Beam Lines at ESRF, Grenoble
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 (creator_code:org_t)
2003-03-06
2003
English.
In: Nature. - : Springer Science and Business Media LLC. - 0028-0836 .- 1476-4687. ; 422:6927, s. 58-61
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The boundary between the Earth's metallic core and its silicate mantle is characterized by strong lateral heterogeneity and sharp changes in density, seismic wave velocities, electrical conductivity and chemical composition(1-7). To investigate the composition and properties of the lowermost mantle, an understanding of the chemical reactions that take place between liquid iron and the complex Mg-Fe-Si-Al-oxides of the Earth's lower mantle is first required(8-15). Here we present a study of the interaction between iron and silica (SiO2) in electrically and laser-heated diamond anvil cells. In a multianvil apparatus at pressures up to 140 GPa and temperatures over 3,800 K we simulate conditions down to the core-mantle boundary. At high temperature and pressures below 40 GPa, iron and silica react to form iron oxide and an iron-silicon alloy, with up to 5 wt% silicon. At pressures of 85-140 GPa, however, iron and SiO2 do not react and iron-silicon alloys dissociate into almost pure iron and a CsCl-structured (B2) FeSi compound. Our experiments suggest that a metallic silicon-rich B2 phase, produced at the core-mantle boundary (owing to reactions between iron and silicate(2,9,10,13)), could accumulate at the boundary between the mantle and core and explain the anomalously high electrical conductivity of this region(6).

Subject headings

TEKNIK OCH TEKNOLOGIER  -- Annan teknik -- Övrig annan teknik (hsv//swe)
ENGINEERING AND TECHNOLOGY  -- Other Engineering and Technologies -- Other Engineering and Technologies not elsewhere specified (hsv//eng)

Keyword

HIGH-PRESSURE; LIQUID-IRON; INNER-CORE; X-RAY; BOUNDARY; TEMPERATURES; METAL; HETEROGENEITY
Material physics with surface physics
Materialfysik med ytfysik

Publication and Content Type

ref (subject category)
art (subject category)

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