Ferromagnetism ofat ambient and high pressure
- 1 May 1987
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 35 (13) , 6880-6887
- https://doi.org/10.1103/physrevb.35.6880
Abstract
We have made detailed investigations of the structural and magnetic properties of (1.0≤x≤2.0). The homogeneity region of the -type (-type) phase is limited to the Si concentrations x: 1.67≤x≤2.0 and does not extend to the concentration range 1.55≤x≤2.0, as was reported previously. A transformation from the tetragonal -type structure to the orthorhombic -type structure appears to occur in the system in the same range (1.84<x<1.9) where ferromagnetism appears and the specific-heat coefficient γ passes through a peak. The presence of an unknown stable phase with composition intermediate to and has been detected. Magnetically ordered ground states have been observed for x≤1.84 and no magnetic or superconducting ordering above 400 mK has been detected for x≥1.90. The present data indicates that magnetism in the system may not be simple ferromagnetic. The experimental behavior of this system appears to be Kondo-lattice-like both at ambient and high pressure.
Keywords
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