journal article·2018-07-01Open access

Spin transition of ferropericlase under shock compression

N. B. Zhang, Y. Cai, X. H. Yao, X. M. Zhou, Y. Y. Li, C. J. Song, X. Y. Qin, S. N. Luo

AIP Advances· Volume 8· Issue 7

Abstract

Planar shock compression experiments are performed at 9–105 GPa on polycrystalline ferropericlase (Mg0.94Fe0.06)O to investigate its Fe2+ spin transition. Forward and reverse impact configurations are used to obtain Hugoniot and shock-state sound velocities. While wave profiles, shock velocity–particle velocity and pressure–density measurements show negligible/weak indications of a phase transition, the shock-state sound speed data clearly manifest a phase transition in the range of 36–62 GPa at the nanosecond time scales. These shock data reveal the phase transition as the spin transition identified in static compression experiments and first-principles calculations.
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Research context

OpenAlex topics: High-pressure geophysics and materials · Geological and Geochemical Analysis · earthquake and tectonic studies

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Affiliations

Department of Engineering Mechanics, South China University of Technology 1 , Guangzhou, Guangdong 510640, P. R. China

Key Laboratory of Advanced Technologies of Materials, Ministry of Education, Southwest Jiaotong University 2 , Chengdu, Sichuan 610031, P. R. China

The Peac Institute of Multiscale Sciences 3 , Chengdu, Sichuan 610031, P. R. China

Key Laboratory of Materials Physics, Institute of Solid State Physics, Chinese Academy of Sciences 4 , Hefei 230031, P. R. China

College of Electronic & information Engineering, Qingdao University 5 , Qingdao 266071, P. R. China

Funding

the Scientific Challenge Project of China

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