Synthesis of New Polytypic Modifications of Fe7C3 at 5.5 GPa

A. I. Chepurov; S. A. Gromilov; V. M. Sonin; E. I. Zhimulev; A. S. Sukhikh; A. A. Chepurov; N. V. Sobolev

doi:10.1134/S1028334X19080191

Synthesis of New Polytypic Modifications of Fe₇C₃ at 5.5 GPa

A. I. Chepurov, S. A. Gromilov, V. M. Sonin, E. I. Zhimulev, A. S. Sukhikh, A. A. Chepurov, N. V. Sobolev

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

Аннотация

The results of experimental synthesis of carbide Fe₇C₃ at 5.5 GPa are presented. It is found that carbide Fe₃C and several polytypes of carbide Fe₇C₃ are formed along with diamond during cooling of the system. It is considered that the Fe₇C₃ phase is a component of the Earth’s inner core. Our results indicate that polytypic carbide modifications could have been formed under natural conditions at relatively low pressures during differentiation of the Earth.

Язык оригинала	английский
Страницы (с-по)	957-959
Число страниц	3
Журнал	Doklady Earth Sciences
Том	487
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X19080191
Состояние	Опубликовано - 1 авг 2019

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10.1134/S1028334X19080191

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@article{55477d01f2f94f1b9f38e6f31ad41075,

title = "Synthesis of New Polytypic Modifications of Fe7C3 at 5.5 GPa",

abstract = "The results of experimental synthesis of carbide Fe7C3 at 5.5 GPa are presented. It is found that carbide Fe3C and several polytypes of carbide Fe7C3 are formed along with diamond during cooling of the system. It is considered that the Fe7C3 phase is a component of the Earth{\textquoteright}s inner core. Our results indicate that polytypic carbide modifications could have been formed under natural conditions at relatively low pressures during differentiation of the Earth.",

keywords = "CARBON, DIAMOND, SYSTEM, IRON, CRYSTALLIZATION",

author = "Chepurov, {A. I.} and Gromilov, {S. A.} and Sonin, {V. M.} and Zhimulev, {E. I.} and Sukhikh, {A. S.} and Chepurov, {A. A.} and Sobolev, {N. V.}",

year = "2019",

month = aug,

day = "1",

doi = "10.1134/S1028334X19080191",

language = "English",

volume = "487",

pages = "957--959",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "PLEIADES PUBLISHING INC",

number = "2",

}

Synthesis of New Polytypic Modifications of Fe₇C₃ at 5.5 GPa. / Chepurov, A. I.; Gromilov, S. A.; Sonin, V. M.; Zhimulev, E. I.; Sukhikh, A. S.; Chepurov, A. A.; Sobolev, N. V.

В: Doklady Earth Sciences, Том 487, № 2, 01.08.2019, стр. 957-959.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

TY - JOUR

T1 - Synthesis of New Polytypic Modifications of Fe7C3 at 5.5 GPa

AU - Chepurov, A. I.

AU - Gromilov, S. A.

AU - Sonin, V. M.

AU - Zhimulev, E. I.

AU - Sukhikh, A. S.

AU - Chepurov, A. A.

AU - Sobolev, N. V.

PY - 2019/8/1

Y1 - 2019/8/1

N2 - The results of experimental synthesis of carbide Fe7C3 at 5.5 GPa are presented. It is found that carbide Fe3C and several polytypes of carbide Fe7C3 are formed along with diamond during cooling of the system. It is considered that the Fe7C3 phase is a component of the Earth’s inner core. Our results indicate that polytypic carbide modifications could have been formed under natural conditions at relatively low pressures during differentiation of the Earth.

AB - The results of experimental synthesis of carbide Fe7C3 at 5.5 GPa are presented. It is found that carbide Fe3C and several polytypes of carbide Fe7C3 are formed along with diamond during cooling of the system. It is considered that the Fe7C3 phase is a component of the Earth’s inner core. Our results indicate that polytypic carbide modifications could have been formed under natural conditions at relatively low pressures during differentiation of the Earth.

KW - CARBON

KW - DIAMOND

KW - SYSTEM

KW - IRON

KW - CRYSTALLIZATION

UR - http://www.scopus.com/inward/record.url?scp=85073226504&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19080191

DO - 10.1134/S1028334X19080191

M3 - Article

AN - SCOPUS:85073226504

VL - 487

SP - 957

EP - 959

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -