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The CaCO3–Fe interaction : Kinetic approach for carbonate subduction to the deep Earth's mantle. / Martirosyan, N. S.; Yoshino, T.; Shatskiy, A. et al.

In: Physics of the Earth and Planetary Interiors, Vol. 259, 01.10.2016, p. 1-9.

Research output: Contribution to journal › Article › peer-review

Harvard

Martirosyan, NS, Yoshino, T, Shatskiy, A, Chanyshev, AD & Litasov, KD 2016, 'The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth's mantle', Physics of the Earth and Planetary Interiors, vol. 259, pp. 1-9. https://doi.org/10.1016/j.pepi.2016.08.008

APA

Martirosyan, N. S., Yoshino, T., Shatskiy, A., Chanyshev, A. D., & Litasov, K. D. (2016). The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth's mantle. Physics of the Earth and Planetary Interiors, 259, 1-9. https://doi.org/10.1016/j.pepi.2016.08.008

Vancouver

Martirosyan NS, Yoshino T, Shatskiy A, Chanyshev AD, Litasov KD. The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth's mantle. Physics of the Earth and Planetary Interiors. 2016 Oct 1;259:1-9. doi: 10.1016/j.pepi.2016.08.008

Author

Martirosyan, N. S. ; Yoshino, T. ; Shatskiy, A. et al. / The CaCO3–Fe interaction : Kinetic approach for carbonate subduction to the deep Earth's mantle. In: Physics of the Earth and Planetary Interiors. 2016 ; Vol. 259. pp. 1-9.

BibTeX

@article{09071e9bafbb4c63be4e9652343d7b97,
title = "The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth's mantle",
abstract = "The CaCO3–Fe0 system, as a model for redox reactions between carbonates and reduced lithologies at the slab-mantle interface during subduction or at core-mantle boundary, was investigated systematically at temperatures from 650 to 1400 °C and pressures from 4 to 16 GPa using multianvil apparatus. CaCO3 reduction via reaction: 3 CaCO3 (aragonite) + 13 Fe0 (metal) = Fe7C3 (carbide) + 3 CaFe2O3 (Ca-w{\"u}stite) was observed. The thickness of the reaction-product layer (Δx) increases linearly with the square root of time in the time-series experiments (t), indicating diffusion-controlled process. The reaction rate constant (k = Δx2/2t) is log-linear relative to 1/T. Its temperature dependences was determined to be k [m2/s] = 2.1 × 10−7exp(−162[kJ/mol]/RT) at 4–6 GPa and k [m2/s] = 2.6 × 10−11exp(−65[kJ/mol]/RT) at 16 GPa. The sluggish kinetics of established CaCO3–Fe0 interaction suggests that significant amount of carbonates could survive during subduction from metal saturation boundary near 250 km depth down to the transition zone and presumably to the lower mantle if melting of carbonates is not involved.",
keywords = "Ca-carbonate, Ca-w{\"u}stite, Iron carbide, Kinetics, Redox reaction, Subducted slab",
author = "Martirosyan, {N. S.} and T. Yoshino and A. Shatskiy and Chanyshev, {A. D.} and Litasov, {K. D.}",
year = "2016",
month = oct,
day = "1",
doi = "10.1016/j.pepi.2016.08.008",
language = "English",
volume = "259",
pages = "1--9",
journal = "Physics of the Earth and Planetary Interiors",
issn = "0031-9201",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - The CaCO3–Fe interaction

T2 - Kinetic approach for carbonate subduction to the deep Earth's mantle

AU - Martirosyan, N. S.

AU - Yoshino, T.

AU - Shatskiy, A.

AU - Chanyshev, A. D.

AU - Litasov, K. D.

PY - 2016/10/1

Y1 - 2016/10/1

N2 - The CaCO3–Fe0 system, as a model for redox reactions between carbonates and reduced lithologies at the slab-mantle interface during subduction or at core-mantle boundary, was investigated systematically at temperatures from 650 to 1400 °C and pressures from 4 to 16 GPa using multianvil apparatus. CaCO3 reduction via reaction: 3 CaCO3 (aragonite) + 13 Fe0 (metal) = Fe7C3 (carbide) + 3 CaFe2O3 (Ca-wüstite) was observed. The thickness of the reaction-product layer (Δx) increases linearly with the square root of time in the time-series experiments (t), indicating diffusion-controlled process. The reaction rate constant (k = Δx2/2t) is log-linear relative to 1/T. Its temperature dependences was determined to be k [m2/s] = 2.1 × 10−7exp(−162[kJ/mol]/RT) at 4–6 GPa and k [m2/s] = 2.6 × 10−11exp(−65[kJ/mol]/RT) at 16 GPa. The sluggish kinetics of established CaCO3–Fe0 interaction suggests that significant amount of carbonates could survive during subduction from metal saturation boundary near 250 km depth down to the transition zone and presumably to the lower mantle if melting of carbonates is not involved.

AB - The CaCO3–Fe0 system, as a model for redox reactions between carbonates and reduced lithologies at the slab-mantle interface during subduction or at core-mantle boundary, was investigated systematically at temperatures from 650 to 1400 °C and pressures from 4 to 16 GPa using multianvil apparatus. CaCO3 reduction via reaction: 3 CaCO3 (aragonite) + 13 Fe0 (metal) = Fe7C3 (carbide) + 3 CaFe2O3 (Ca-wüstite) was observed. The thickness of the reaction-product layer (Δx) increases linearly with the square root of time in the time-series experiments (t), indicating diffusion-controlled process. The reaction rate constant (k = Δx2/2t) is log-linear relative to 1/T. Its temperature dependences was determined to be k [m2/s] = 2.1 × 10−7exp(−162[kJ/mol]/RT) at 4–6 GPa and k [m2/s] = 2.6 × 10−11exp(−65[kJ/mol]/RT) at 16 GPa. The sluggish kinetics of established CaCO3–Fe0 interaction suggests that significant amount of carbonates could survive during subduction from metal saturation boundary near 250 km depth down to the transition zone and presumably to the lower mantle if melting of carbonates is not involved.

KW - Ca-carbonate

KW - Ca-wüstite

KW - Iron carbide

KW - Kinetics

KW - Redox reaction

KW - Subducted slab

UR - http://www.scopus.com/inward/record.url?scp=84984652094&partnerID=8YFLogxK

U2 - 10.1016/j.pepi.2016.08.008

DO - 10.1016/j.pepi.2016.08.008

M3 - Article

AN - SCOPUS:84984652094

VL - 259

SP - 1

EP - 9

JO - Physics of the Earth and Planetary Interiors

JF - Physics of the Earth and Planetary Interiors

SN - 0031-9201

ER -

ID: 25789602