Ferrimagnetic spiral configurations in cobalt chromite

N. Menyuk, K. Dwight, A. Wold
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引用次数: 120

Abstract

Cobalt chromite, CoCr2O4, is a cubic spinel which is ferrimagnetic at low temperatures with a Curie point Tc ≈ 97 °K. The room temperature powder diffraction pattern on this material, corrected for temperature effects, shows that it is a normal spinel with an oxygen parameter equal to 0.38707 :f: .00005. At 4.2 °K there are, in addition to the magnetic contributions to the fundamental spinel peaks, a large number of magnetic 11 satellite " peaks. All of the additional peaks can be indexed on the basis of the ferrimagnetic spiral model proposed for normal cubic spinels by Lyons, Kaplan, Dwight and Menyuk, in which the spiraling components of the spins are defined by a single k vector along a face diagonal. The experimental magnitude of |k| is approximately 5 % greater than theoretically predicted. The neutron diffraction pattern predicted on the basis of the spiral model is completely determined upon fixing the exchange ratio JBB/J AB and the cone axis direction. Taking JBB /J AB = 1. 5 on the basis of magnetization measurements previously reported, it is found that the intensities of the various peaks are in excellent agreement with the intensities predicted by the spiral model with the cone axis along an [001] direction. The ferrimagnetic spiral configuration is known to become unstable relative to small deviations for JBB SB /JAB S A > 0.98 (i.e. JBB/JAB > 0.98 in CoCr2O4). However, our results indicate that the true configuration closely approximates that predicted by the model over a range of exchange interaction ratios which extends well beyond the onset of local instability. Upon increasing the temperature above 4,2 °K, the satellite peaks disappeared between 25 °K and 35 °K, apparently degenerating into a broad plateau observed at 50 °K and 77 °K. Despite this disappearance, a self-consistent fit to neither the magnetic contributions to the fundamental peaks nor the observed thermal variation of the magnetization can be obtained from a collinear model. However, the predicted values based on a molecular field treatment of the spiral model are in good agreement with these measurements. These results further corroborate the validity of the spiral model for CoCr2O4, and indicate that the molecular field approximation accurately describes the axial component throughout its ferrimagnetic range, but not the azimuthal component.
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钴铬铁矿中的铁磁螺旋结构
CoCr2O4是一种立方尖晶石,在低温下具有铁磁性,居里点Tc≈97°K。对该材料的室温粉末衍射图进行了温度影响校正,结果表明该材料为正常尖晶石,氧参数为0.38707:f: 0.00005。在4.2°K处,除了磁性对基本尖晶石峰的贡献外,还有大量的磁性11卫星峰。根据Lyons、Kaplan、Dwight和Menyuk提出的正常立方尖晶石的铁磁螺旋模型,所有的附加峰都可以被索引,其中自旋的螺旋分量由沿面对角线的单个k矢量定义。实验值比理论预测值大约大5%。在确定交换比JBB/ jab和锥轴方向后,完全确定了基于螺旋模型预测的中子衍射图。令JBB / jab = 1。5根据先前报道的磁化测量,发现各峰的强度与沿[001]方向的锥轴螺旋模型预测的强度非常一致。已知当JBB SB /JAB sa > 0.98(即CoCr2O4中JBB/JAB > 0.98)时,相对于较小的偏差,铁磁螺旋结构变得不稳定。然而,我们的结果表明,在交换相互作用比的范围内,真实的结构与模型预测的非常接近,该范围远远超出了局部不稳定的开始。当温度高于4.2°K时,卫星峰在25°K和35°K之间消失,在50°K和77°K时明显退化为一个广阔的高原。尽管这种消失,但从共线模型中既不能得到对基波峰的磁贡献,也不能得到观测到的磁化强度的热变化的自洽拟合。然而,基于螺旋模型的分子场处理的预测值与这些测量结果很好地吻合。这些结果进一步证实了CoCr2O4螺旋模型的有效性,并表明分子场近似准确地描述了CoCr2O4在整个铁磁范围内的轴向分量,而不是方位角分量。
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