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Electronic topological transitions, magnetic ordering and the Fermi surfaces of Y and the heavy rare earths

机译:Y和重稀土的电子拓扑转变,磁有序性和费米面

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The magnetic order of the heavy rare earths has long been associated with the presence of a certain feature in the Fermi surface (FS) topology (being common to non-magnetic Y also), known as the "webbing". Furthermore, there has been speculation that changes in the observed ordering, brought about by temperature-induced changes in the crystalline c/a ratio, are due to the presence or absence of that webbing feature. Such a simplistic model is appealingly simple in systems where physics of the exchange interaction as a function of composition and temperature is complicated. The Gd1-xYx alloy system exhibits ferromagnetism or helical antiferromagnetism at different compositions and temperatures. We present our experimental measurement of the FS topology of such an alloy at a composition close to the Y concentration where helical antiferromagnetism occurs. The data show that the evolution of the FS in Gd1-xYx is different from that predicted by the model based on the c/a ratio, suggesting a less simplistic interpretation. [References: 30]
机译:长期以来,重稀土的磁性顺序与费米表面(FS)拓扑中某些特征(也与非磁性Y相同)的存在相关联,被称为“织带”。此外,已经推测,由温度引起的结晶c / a比变化引起的观察到的有序变化是由于存在或不存在织带特征引起的。这种简单的模型在交换相互作用的物理过程(取决于组成和温度)复杂的系统中非常简单。 Gd1-xYx合金系统在不同的成分和温度下表现出铁磁性或螺旋反铁磁性。我们介绍了这种合金的FS拓扑的实验测量结果,该合金的成分接近Y浓度(发生螺旋反铁磁性)。数据表明Gd1-xYx中FS的演化与模型基于c / a比率预测的演化不同,这表明解释的简化程度较低。 [参考:30]

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