Ga-substituted cobalt ferrite oxides show promise as high magnetostriction, high sensitivity magnetoelastic materials for sensor and actuator applications, but their atomic-level behavior is not yet well understood. In this study, the magnetic environments of the Fe atoms in Ga-substituted cobalt ferrite have been investigated using Mossbauer spectroscopy. A series of five powder samples with CoGa x Fe 2−x O 4 compositions ͑x = 0.0-0.8͒ was investigated using transmission geometry. Results show two distinct six-line hyperfine patterns, which are identified as Fe in A ͑tetrahedral͒ and B ͑octahedral͒ spinel sites. Increasing Ga concentration is seen to decrease the hyperfine field strength for both A and B sites, as well as increasing the width of those distributions, consistent with the nonmagnetic nature of Ga 3+ ions. Effects are more pronounced for the B sites than the A sites. Results for Ga substitution show more pronounced effects than for previous studies with Cr 3+ or Mn 3+ substitution: the hyperfine fields decrease and distribution widths increase at greater rates, and the differences between A and B site behavior are more pronounced. Results indicate that at least for the lower Ga concentrations, the Ga 3+ ions substitute predominantly into the A sites, in contrast to Cr 3+ and Mn 3+ which substitute into the B sites. This interpretation is supported by measurements of magnetization at low temperatures. © 2008 American Institute of Physics. ͓DOI: 10.1063/1.2834721͔
INTRODUCTIONThe development of cobalt ferrite-based materials has received recent attention for the potential applicability of such materials as magnetoelastic sensors and actuators, and as the magnetoelastic component in composite "multiferroics." 1,2 Substitution of elements such as Mn or Cr for some of the Fe has shown promise of adjusting the magnetic and magnetoelastic properties of these materials through control of chemical composition. 3,4 In order to fully enable the practical applications of these compounds, a more complete family of materials is needed, such that the desired properties can be tailored to a specific application. In the present study, we report on the magnetic characterization of the series of Ga-substituted cobalt ferrites CoGa x Fe 2−x O 4 ͑x = 0.0-0.8͒ as a function of gallium concentration using transmission Mossbauer spectroscopy. The effects of this substitution were expected to be different for Mn and Cr substitution. [5][6][7]
EXPERIMENTAL DETAILSThe samples used in this study were prepared at Ames Laboratory, USDOE. The samples were of the composition CoGa x Fe 2−x O 4 ͑where x = 0.0-0.8͒. Standard powder ceramic techniques were employed using Fe 2 O 3 , Ga 2 O 3 , and Co 3 O 4 powders as precursors. The powders were calcined twice, sintered at 1350°C for 24 h, and furnace cooled ͑see Ref. 7 for details͒. The final compositions of the samples were determined by energy-dispersive x-ray spectroscopy, and all samples were confirmed by x-ray powder diffractometry to be single phase and have the cubic spinel ...