Abstract
For iron-sulfide (FeS), we investigate the correlation between the structural details, including its dimensionality and composition, with its magnetic and superconducting properties. We compare, theoretically and experimentally, the two-dimensional (2D) layered tetragonal (“t-FeS”) phase with the 3D hexagonal (“h-FeS”) phase. X-ray diffraction reveals iron-deficient chemical compositions of t-Fe0.93(1)S and h-Fe0.84(1)S that show no low-temperature structural transitions. First-principles calculations reveal a high sensitivity of the 2D structure to the electronic and magnetic properties, predicting marginal antiferromagnetic instability for our compound (sulfur height of zS = 0.252) with an ordering energy of about 11 meV/Fe, while the 3D phase is magnetically stable. Experimentally, h-Fe0.84S orders magnetically well above room temperature, while t-Fe0.93S shows coexistence of antiferromagnetism at TN = 116 and filamentary superconductivity below Tc = 4 K. Low temperature neutron diffraction data reveals antiferromagnetic commensurate ordering with wave vector km = (0.25,0.25,0) and 0.46(2) µB/Fe. Additionally, neutron scattering measurements were used to find the particle size and iron vacancy arrangement of t-FeS and h-FeS. The structure of iron sulfide has a delicate relationship with the superconducting transition; while our sample with a = 3.6772(7) Å is a filamentary superconductor coexisting with an antiferromagnetic phase, previously reported samples with a > 3.68 Å are bulk superconductors with no magnetism, and those with a ≈ 3.674 Å show magnetic properties.
Original language | English |
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Pages (from-to) | 29-36 |
Number of pages | 8 |
Journal | Physica C: Superconductivity and its Applications |
Volume | 534 |
DOIs | |
State | Published - Mar 15 2017 |
Funding
S.K. would like to acknowledge DOE Office of Science Graduate Student Research Program award for funding, which is administered by the Oak Ridge Institute for Science and Education for the Department of Energy under contract number DE-AC05-06OR23100. This work was primarily supported by the U.S. Department of Energy (DOE), Office of Science, Basic Energy Sciences (BES), Materials Science and Engineering Division (M.M, D.P. L.L, and A.S.) and Chemical Sciences, Geosciences, and Biosciences Division (M.K.K.). The work at ORNL's High Flux Isotope Reactor (HFIR) was sponsored by the Scientific User Facilities Division, Office of BES, U.S. DOE (C.D. and L.D.). This study was partially funded (W.C.) by ORNL's Lab-Directed Research & Development of the Wigner Fellowship program. M.K. acknowledges Chemical Sciences, Geosciences, and Biosciences Division. J.E. would like to acknowledge Higher Education Research Experiences ‘HERE’ Program, as well as Ruth Ann Verell representing Allegheny College, for his summer-student opportunity at ORNL. MRE acknowledges support by the U.S. Department of Energy, Office of Basic Energy Sciences, under Awards No. DE-FG02-10ER46783.
Funders | Funder number |
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HFIR | |
ORNL's High Flux Isotope Reactor | |
ORNL's Lab-directed Research & Development | |
Office of BES | |
Ruth Ann Verell representing Allegheny College | |
Scientific User Facilities Division | |
U.S. Department of Energy | DE-AC05-06OR23100 |
Office of Science | |
Basic Energy Sciences | DE-FG02-10ER46783 |
Oak Ridge National Laboratory | |
Oak Ridge Institute for Science and Education | |
Division of Materials Sciences and Engineering | |
Chemical Sciences, Geosciences, and Biosciences Division |