1998
DOI: 10.1016/s0151-9107(98)80078-0
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Unusual magnetic behavior in LaFeCrO

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Cited by 19 publications
(15 citation statements)
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“…The fact that these values are similar indicates that the Fe/Cr valences in both samples are identical, which is consistent with the stabilization of the <Fe/Cr-O> for these two samples (Figure 2). As shown in Figure 6, where previously reported results for LaFeO 3 16 and SrFeO 2.95 19 were included for comparison purposes, there is a monotonic decrease of T ord with the increase of <r A > (which mimics the Sr content) for x e 0.6. This trend is broken for x g 0.8, indicating that a different charge compensation mechanism appears in this case, corroborating the previous suggestion (see structural discussion) of an increased role for oxygen vacancy formation on the overall charge compensation regime.…”
Section: Resultsmentioning
confidence: 71%
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“…The fact that these values are similar indicates that the Fe/Cr valences in both samples are identical, which is consistent with the stabilization of the <Fe/Cr-O> for these two samples (Figure 2). As shown in Figure 6, where previously reported results for LaFeO 3 16 and SrFeO 2.95 19 were included for comparison purposes, there is a monotonic decrease of T ord with the increase of <r A > (which mimics the Sr content) for x e 0.6. This trend is broken for x g 0.8, indicating that a different charge compensation mechanism appears in this case, corroborating the previous suggestion (see structural discussion) of an increased role for oxygen vacancy formation on the overall charge compensation regime.…”
Section: Resultsmentioning
confidence: 71%
“…In fact, both LaCrO 3 and LaFeO 3 are antiferromagnetic materials with Néel temperatures of ∼280 and 750 K, respectively. 16 In the substituted sample a ferromagnetic component due to the Fe 3+ (d 5 )-O-Cr 3+ (d 3 ) interaction was expected, although not observed. However, it was previously reported 17 that this effect would be observed only if the bond angle at the intervening anion was sufficiently close to 180°, which is not the present case (Table 4).…”
Section: Resultsmentioning
confidence: 83%
“…In particular, the replacement of Fe 3+ by Cr 3+ and its effect on structural, magnetic and other properties have been reported [5][6][7] for rare earth orthoferrites. For example, in the lanthanum orthoferrites, partial replacement of Fe by Cr leads to a reduction in the Néel temperature from 750 K in LaFeO 3 to 280 K in LaCrO 3 .…”
Section: Introductionmentioning
confidence: 99%
“…Combining the structural analysis of Fe-O and the FT spectra, our results indicate that ferromagnetic coupling of Fe-O-Cr is present and phase separation is not the real reason for the absence of FM in the LaFe 1-x Cr x O 3 sample. In another paper (Belayachi et al, 1998), the authors found an unusual magnetic behaviour in LaFe 1-x Cr x O 3 when x > 0.5. In Fig.…”
Section: Testing Using the Lafe 1-x Cr X O 3 Systemmentioning
confidence: 93%
“…As a result, a ferromagnetic-ordered phase has not been obtained. In this work, powder samples of LaFe 1-x Cr x O 3 (x = 0, 1/3, 2/3) were synthesized using a standard solid-state reaction method (Belayachi et al, 1996;Louca et al, 1999). X-ray diffraction spectra indicated that all samples crystallize in the perovskite structure with orthorhombic deformation, having a space group Pbnm (Wang et al, 2007).…”
Section: Testing Using the Lafe 1-x Cr X O 3 Systemmentioning
confidence: 99%