Mechanism and kinetics of the post-spinel transformation in Mg2SiO4

Tomoaki Kubo, Eiji Ohtani, Takumi Kato, Satoru Urakawa, Akio Suzuki, Yuichi Kanbe, Ken Ichi Funakoshi, Wataru Utsumi, Takumi Kikegawa, Kiyoshi Fujino

Research output: Contribution to journalArticle

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Abstract

Mechanisms and kinetics of the post-spinel transformation in Mg2SiO4 were examined at 22.7-28.2 GPa and 860-1200°C by in situ X-ray diffraction experiments using synchrotron radiation combined with microstructural observations of the recovered samples. The post-spinel phases nucleated on spinel grain boundaries and grew with a lamellar texture. Under large overpressure conditions, reaction rims were formed along spinel grain boundaries at the initial stage of the transformation, whereas under small overpressure conditions, the transformation proceeded without formation of reaction rims. Mg2SiO4 spinel metastably dissociated into MgSiO3 ilmenite and periclase, and stishovite and periclase as intermediate steps in the transformation into the stable assemblage of MgSiO3 perovskite and periclase. Topotactic relationships were found in the transformation from spinel into ilmenite and periclase. Kinetic parameters in the Avrami rate equation, time taken to 10% completion, and the growth rate were estimated by analysis of the kinetic data obtained by in situ X-ray observations. The empirical activation energy for 10% transformation decreases with increasing pressure because the activation energy for nucleation becomes smaller at larger overpressure conditions. Extrapolations of the 10% transformation to ∼700°C, which is the lowest temperature expected for the cold slabs at ∼700 km depth, suggest that overpressure of more than ∼1 GPa is needed for the transformation. Because the growth rate is estimated to be large even at low-temperatures of ∼700°C and overpressures of 1 GPa, the depth of the post-spinel transformation in the cold slabs is possibly controlled by nucleation kinetics.

Original languageEnglish
Pages (from-to)153-171
Number of pages19
JournalPhysics of the Earth and Planetary Interiors
Volume129
Issue number1-2
DOIs
Publication statusPublished - Jan 1 2002

Fingerprint

spinel
overpressure
periclase
kinetics
ilmenite
grain boundary
rims
activation energy
nucleation
slab
slabs
grain boundaries
stishovite
perovskite
extrapolation
synchrotron radiation
x rays
textures
texture
X-ray diffraction

All Science Journal Classification (ASJC) codes

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

Cite this

Mechanism and kinetics of the post-spinel transformation in Mg2SiO4 . / Kubo, Tomoaki; Ohtani, Eiji; Kato, Takumi; Urakawa, Satoru; Suzuki, Akio; Kanbe, Yuichi; Funakoshi, Ken Ichi; Utsumi, Wataru; Kikegawa, Takumi; Fujino, Kiyoshi.

In: Physics of the Earth and Planetary Interiors, Vol. 129, No. 1-2, 01.01.2002, p. 153-171.

Research output: Contribution to journalArticle

Kubo, T, Ohtani, E, Kato, T, Urakawa, S, Suzuki, A, Kanbe, Y, Funakoshi, KI, Utsumi, W, Kikegawa, T & Fujino, K 2002, 'Mechanism and kinetics of the post-spinel transformation in Mg2SiO4 ', Physics of the Earth and Planetary Interiors, vol. 129, no. 1-2, pp. 153-171. https://doi.org/10.1016/S0031-9201(01)00270-9
Kubo, Tomoaki ; Ohtani, Eiji ; Kato, Takumi ; Urakawa, Satoru ; Suzuki, Akio ; Kanbe, Yuichi ; Funakoshi, Ken Ichi ; Utsumi, Wataru ; Kikegawa, Takumi ; Fujino, Kiyoshi. / Mechanism and kinetics of the post-spinel transformation in Mg2SiO4 In: Physics of the Earth and Planetary Interiors. 2002 ; Vol. 129, No. 1-2. pp. 153-171.
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