Magnetic tricritical point and nematicity in FeSe under pressure

Rustem Khasanov, Rafael M. Fernandes, Gediminas Simutis, Zurab Guguchia, Alex Amato, Hubertus Luetkens, Elvezio Morenzoni, Xiaoli Dong, Fang Zhou, Zhongxian Zhao

Research output: Contribution to journalArticlepeer-review

10 Scopus citations

Abstract

Magnetism induced by external pressure (p) was studied in a FeSe crystal sample by means of muon-spin rotation. The magnetic transition changes from second order to first order for pressures exceeding the critical value pc≃2.4-2.5 GPa. The magnetic ordering temperature (TN) and the value of the magnetic moment per Fe site (mFe) increase continuously with increasing pressure, reaching TN≃50 K and mFe≃0.25μB at p≃2.6 GPa, respectively. No pronounced features at both TN(p) and mFe(p) are detected at p≃pc, thus suggesting that the stripe-type magnetic order in FeSe remains unchanged above and below the critical pressure pc. A phenomenological model for the (p,T) phase diagram of FeSe reveals that these observations are consistent with a scenario where the nematic transitions of FeSe at low and high pressures are driven by different mechanisms.

Original languageEnglish (US)
Article number224510
JournalPhysical Review B
Volume97
Issue number22
DOIs
StatePublished - Jun 13 2018

Bibliographical note

Funding Information:
This work was performed at the Swiss Muon Source (), Paul Scherrer Institute (PSI, Switzerland). R.M.F. is supported by the U. S. Department of Energy, Office of Science, Basic Energy Sciences, under Award No. DE-SC0012336. The work of G.S. is supported by the Swiss National Science Foundation, Grants No. 200021_149486 and No. 200021_175935. The work of X.D., F.Z., and Z.Z. was supported by the “National Key Research and Development Program of China (Grant No. 2016YFA0300301),” the “Strategic Priority Research Program (B)” of the Chinese Academy of Sciences (Grant No. XDB07020100), and the Natural Science Foundation of China (Grant No. 11574370).

Fingerprint Dive into the research topics of 'Magnetic tricritical point and nematicity in FeSe under pressure'. Together they form a unique fingerprint.

Cite this