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Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa : a study by in situ X-ray diffraction. / Litasov, K. D.; Shatskiy, A. F.; Ohtani, E.

In: Geochemistry International, Vol. 54, No. 10, 01.10.2016, p. 914-921.

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

Harvard

Litasov, KD, Shatskiy, AF & Ohtani, E 2016, 'Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa: a study by in situ X-ray diffraction', Geochemistry International, vol. 54, no. 10, pp. 914-921. https://doi.org/10.1134/S0016702916100074

APA

Litasov, K. D., Shatskiy, A. F., & Ohtani, E. (2016). Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa: a study by in situ X-ray diffraction. Geochemistry International, 54(10), 914-921. https://doi.org/10.1134/S0016702916100074

Vancouver

Litasov KD, Shatskiy AF, Ohtani E. Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa: a study by in situ X-ray diffraction. Geochemistry International. 2016 Oct 1;54(10):914-921. doi: 10.1134/S0016702916100074

Author

Litasov, K. D. ; Shatskiy, A. F. ; Ohtani, E. / Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa : a study by in situ X-ray diffraction. In: Geochemistry International. 2016 ; Vol. 54, No. 10. pp. 914-921.

BibTeX

@article{083d869a3bcc44309d7c53bc1a372e43,
title = "Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa: a study by in situ X-ray diffraction",
abstract = "A method of in situ X-ray diffraction at Spring-8 (Japan) was used to analyze simultaneously the hydrogen incorporation into Fe and Fe3C, as well as to measure the relative stability of carbides, nitrides, sulfides, and hydrides of iron at pressures of 6–20 GPa and temperatures up to 1600 K. The following stability sequence of individual iron compounds was established in the studied pressure and temperature interval: FeS > FeN > FeC > FeH > Fe. A change in the unit-cell volume as compared to the known equations of state was used to estimate the hydrogen contents in carbide Fe3C and hydride FeHx. Data on hydride correspond to stoichiometry with x ≈ 1. Unlike iron sulfides and silicides, the solubility of hydrogen in Fe3C seemed to be negligibly low—within measurement error. Extrapolating obtained data to pressures of the Earth{\textquoteright}s core indicates that carbon and hydrogen are mutually incpompatible in the iron–nickel core, while nitrogen easily substitutes carbon and may be an important component of the inner core in the light of the recent models assuming the predominance of iron carbide in its composition.",
keywords = "carbide, experiment, high pressure, hydride, iron, nitride, X-ray diffraction",
author = "Litasov, {K. D.} and Shatskiy, {A. F.} and E. Ohtani",
year = "2016",
month = oct,
day = "1",
doi = "10.1134/S0016702916100074",
language = "English",
volume = "54",
pages = "914--921",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "PLEIADES PUBLISHING INC",
number = "10",

}

RIS

TY - JOUR

T1 - Interaction of Fe and Fe3C with hydrogen and nitrogen at 6–20 GPa

T2 - a study by in situ X-ray diffraction

AU - Litasov, K. D.

AU - Shatskiy, A. F.

AU - Ohtani, E.

PY - 2016/10/1

Y1 - 2016/10/1

N2 - A method of in situ X-ray diffraction at Spring-8 (Japan) was used to analyze simultaneously the hydrogen incorporation into Fe and Fe3C, as well as to measure the relative stability of carbides, nitrides, sulfides, and hydrides of iron at pressures of 6–20 GPa and temperatures up to 1600 K. The following stability sequence of individual iron compounds was established in the studied pressure and temperature interval: FeS > FeN > FeC > FeH > Fe. A change in the unit-cell volume as compared to the known equations of state was used to estimate the hydrogen contents in carbide Fe3C and hydride FeHx. Data on hydride correspond to stoichiometry with x ≈ 1. Unlike iron sulfides and silicides, the solubility of hydrogen in Fe3C seemed to be negligibly low—within measurement error. Extrapolating obtained data to pressures of the Earth’s core indicates that carbon and hydrogen are mutually incpompatible in the iron–nickel core, while nitrogen easily substitutes carbon and may be an important component of the inner core in the light of the recent models assuming the predominance of iron carbide in its composition.

AB - A method of in situ X-ray diffraction at Spring-8 (Japan) was used to analyze simultaneously the hydrogen incorporation into Fe and Fe3C, as well as to measure the relative stability of carbides, nitrides, sulfides, and hydrides of iron at pressures of 6–20 GPa and temperatures up to 1600 K. The following stability sequence of individual iron compounds was established in the studied pressure and temperature interval: FeS > FeN > FeC > FeH > Fe. A change in the unit-cell volume as compared to the known equations of state was used to estimate the hydrogen contents in carbide Fe3C and hydride FeHx. Data on hydride correspond to stoichiometry with x ≈ 1. Unlike iron sulfides and silicides, the solubility of hydrogen in Fe3C seemed to be negligibly low—within measurement error. Extrapolating obtained data to pressures of the Earth’s core indicates that carbon and hydrogen are mutually incpompatible in the iron–nickel core, while nitrogen easily substitutes carbon and may be an important component of the inner core in the light of the recent models assuming the predominance of iron carbide in its composition.

KW - carbide

KW - experiment

KW - high pressure

KW - hydride

KW - iron

KW - nitride

KW - X-ray diffraction

UR - http://www.scopus.com/inward/record.url?scp=84990963144&partnerID=8YFLogxK

U2 - 10.1134/S0016702916100074

DO - 10.1134/S0016702916100074

M3 - Article

AN - SCOPUS:84990963144

VL - 54

SP - 914

EP - 921

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 10

ER -

ID: 25789347