(Fe,Ni)2P Allabogdanite can be an Ambient Pressure Phase in Iron Meteorites | Sciact - CRIS-система Института катализа

(Fe,Ni)2P Allabogdanite can be an Ambient Pressure Phase in Iron Meteorites Научная публикация

Журнал

Scientific Reports
, E-ISSN: 2045-2322

Вых. Данные

Год: 2020, Том: 10, Номер: 1, Номер статьи : 8956, Страниц : 11 DOI: 10.1038/s41598-020-66039-0

Ключевые слова

Magnetocaloric Effects; Magnetic Refrigeration; Polysilicon

Авторы

Litasov Konstantin D. ¹ , Bekker Tatyana B. ^2,3,4 , Sagatov Nursultan E. ^2,3 , Gavryushkin Pavel N. ^2,3 , Krinitsin PavelG. ^2,3 , Kuper Konstantin E. ⁵

Организации

1	Vereshchagin Institute for High Pressure Physics RAS, Troitsk, Moscow, 108840, Russia
2	Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, 630090, Russia
3	Novosibirsk State University, Novosibirsk, 630090, Russia
4	Novosibirsk State University of Architecture, Design and Arts, Novosibirsk, 630099, Russia
5	Budker Institute of Nuclear Physics, Siberian Branch Russian Academy of Sciences

An orthorhombic modification of (Fe,Ni)2P, allabogdanite, found in iron meteorites was considered to be thermodynamically stable at pressures above 8 GPa and temperatures of 1673 K according to the results of recent static high-pressure and high-temperature experiments. A hexagonal polymorphic modification of (Fe,Ni)2P, barringerite, was considered to be stable at ambient conditions. Experimental investigation through the solid-state synthesis supported by ab initio calculations was carried out to clarify the stability fields of (Fe,Ni)2P polymorphs. Both experimental and theoretical studies show that Fe2P-allabogdanite is a low-temperature phase stable at ambient conditions up to a temperature of at least 773 K and, therefore, is not necessarily associated with high pressures. This is consistent with the textural relationships of allabogdanite in iron meteorites. © 2020, The Author(s).

Litasov K.D. , Bekker T.B. , Sagatov N.E. , Gavryushkin P.N. , Krinitsin P. , Kuper K.E.
(Fe,Ni)2P Allabogdanite can be an Ambient Pressure Phase in Iron Meteorites

Scientific Reports. 2020. V.10. N1. 8956 :1-11. DOI: 10.1038/s41598-020-66039-0 WOS Scopus РИНЦ CAPlus OpenAlex

Полный текст от издателя

Поступила в редакцию:	14 окт. 2019 г.
Принята к публикации:	14 мая 2020 г.
Опубликована online:	2 июн. 2020 г.
Опубликована в печати:	1 дек. 2020 г.

Web of science:	WOS:000560797800018
Scopus:	2-s2.0-85085908505
РИНЦ:	43291967
Chemical Abstracts:	2020:1098715
OpenAlex:	W3030540920

БД	Цитирований
Web of science	13
Scopus	13
OpenAlex	13