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Title: Phase analysis and magnetic properties of RTiFe sub 11 minus x Co sub x (R=Y,Gd) ( x =0--11)

Journal Article · · Journal of Applied Physics; (USA)
DOI:https://doi.org/10.1063/1.347963· OSTI ID:5492861
; ; ; ;  [1]
  1. Metallurgical Engineering and Materials Science Department, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213 (USA)

Both as-cast and 1000 {degree}C annealed RTiFe{sub 11} samples are nearly single phase with a small amount of Fe{sub 2}Ti. Small amounts of Co additions do not change the microstructure, but the minor phase changed to a Fe,Co,Ti solid solution. At high Co concentration, as-cast samples are multiphase (1-12, 2-17, (Fe,Co,Ti)) and high-temperature ({similar to}1200 {degree}C) annealing is needed in order to produce a single-phase microstructure. Results of x-ray analysis and magnetic measurements show that YTiFe{sub 11}, YTiCo{sub 11}, GdTiFe{sub 11}, and GdTiCo{sub 11} are uniaxial and their anisotropy fields at room temperature are 22, 18, 33, and 25 kOe, respectively. Therefore, Fe and Co sublattices are uniaxial with Fe sublattice anisotropy stronger than that of Co. In the intermediate range of composition, there is a conical-planar region for both Y and Gd systems and spin reorientations with temperature were observed. In general, the anisotropy behavior of the RTiFe{sub 11{minus}{ital x}}Co{sub {ital x}} systems (R=Y,Gd) is similar but opposite to their counterpart of R{sub 2}Fe{sub 17{minus}{ital x}}Co{sub {ital x}}. This is due to the similarity of their crystal structure, as both are derivatives of 1-5. However, the strong contribution from the {ital K}{sub 2} anisotropy constant makes the anisotropy phase diagrams of 1-12 more complicated than those of 2-17.

OSTI ID:
5492861
Journal Information:
Journal of Applied Physics; (USA), Vol. 69:8; ISSN 0021-8979
Country of Publication:
United States
Language:
English