We have investigated the magnetic and magnetoelasticproperties of a series of Cr-substituted cobaltferriteCoCrxFe2−xO4 (x=0.0-0.79) samples. Substitution of Cr for some of the Fe in cobaltferrite reduced the Curie temperature, and the effect is more pronounced than that observed in Mn-substituted cobaltferrite samples. Cr substitution also caused the maximum magnetostriction to decrease at a greater rate than substitution of the same amount of Mn. The maximum of the strain derivative, dλ/dH, was reached for x=0.38. The behavior of the Curie temperature of Cr-substituted and Mn-substituted cobaltferrites has been analyzed using the Néel molecular field model and compared with recent Mössbauer spectroscopy results. We have investigated the magnetic and magnetoelastic properties of a series of Cr-substituted cobalt ferrite CoCr x Fe 2−x O 4 ͑x = 0.0-0.79͒ samples. Substitution of Cr for some of the Fe in cobalt ferrite reduced the Curie temperature, and the effect is more pronounced than that observed in Mn-substituted cobalt ferrite samples. Cr substitution also caused the maximum magnetostriction to decrease at a greater rate than substitution of the same amount of Mn. The maximum of the strain derivative, d / dH, was reached for x = 0.38. The behavior of the Curie temperature of Cr-substituted and Mn-substituted cobalt ferrites has been analyzed using the Néel molecular field model and compared with recent Mössbauer spectroscopy results.
IntroductionCobalt ferrite and cobalt ferrite based composites have high magnetoelastic sensitivity, high magnetostriction and low cost, making the materials attractive for use in magnetoelastic sensors [1]. However, to enable practical applications a family of materials is needed, in which the magnetoelastic response, magnetic properties, and their temperature dependences can be tailored by adjusting the chemical composition, microstructure and site occupancies of cations. A series of Mn-substituted cobalt ferrite CoMn x Fe 2-x O 4 has recently been investigated for this purpose and showed promising results [2]. In the present study, a family of Cr-substituted cobalt ferrite CoCr x Fe 2-x O 4 is investigated. The results show that Cr substitution has more profound effects on the Curie temperature and magnetoelastic properties of cobalt ferrite than does Mn substitution. Experimental details and results A series of polycrystalline chromium-substituted cobalt ferrite samples with compositions of CoCr x Fe 2-x O 4 (where x ranges from 0 to 0.8) were prepared by standard powder ceramic techniques [1, 2]. The microstructure and final composition of the samples were characterized using a scanning electron microscope with energy-dispersive x-ray spectroscopy (EDX). The crystal structure of the samples was determined by x-ray diffractometry to be cubic spinel. Curie temperature, T C , was determined by measuring magnetization as a function of temperature in a vibrating sample magnetometer (VSM). Magnetostriction as a function of applied field was measured using the strain gauge method. These results are presented in Fig. 1. Discussion and ConclusionsAs Cr is substituted for Fe in CoCr x Fe 2-x O 4 , the Curie temperature T C decreases with increasing Cr content (Fig. 1b). This effect can be used to adjust magnetic properties through their temperature dependence. In fact, T C decreases at a somewhat greater rate with Cr substitution than with Mn substitution. The magnitude of magnetostriction also decreases with increasing Cr content for values of x up to 0.6 (Fig. 1a). For x = 0.6 magnetostriction becomes positive for fields above 2.5 kOe (200 kA/m), and for x = 0.8 magnetostriction is positive for all fields. Pure cobalt ferrite (x=0) is known to have <100> easy axes, λ 100 <0<λ 111 , and |λ 100 |> |λ 111 | [3]. Thus it appears that substitution of Cr progressively decreases λ 100 relative to λ 111 . Cr substitution also causes the maximum magnetostriction magnitude to decrease at a much greater rate than does Mn substitution (Fig. 1b). Both Cr 3+ and Mn 3+ are known to have strong preference for the octahedral sites in the ferrite structure [4], and Co 2+ has a stronger preference for the octahedral sites than Fe 3+ in pure cobalt ferrite. However, our Mossbauer spectroscopy investigations of these two series of samples appear to indicate that substitution of Cr or Mn for Fe in cobalt ferrite is not a simple substitution of one cation for the other on the octahedral sites [5,6]. Rather, it appears that Cr or Mn substi...
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