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Spin ice in a field: Quasi-phases and pseudo-transitions

机译:在田间旋转冰:准相和伪跃迁

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摘要

Thermodynamics of a short-range model of spin ice magnets in a field is considered in the Bethe-Peierls approximation. The results obtained for [111], [100], and [011] fields agree reasonably well with the existing Monte Carlo simulations and some experiments. In this approximation, all extremely sharp field-induced anomalies are described by analytic functions of temperature and the applied field. In spite of the absence of true phase transitions, the analysis of the entropy and specific heat reliefs over the H-T plane allows discerning "pseudo-phases" with a specific character of spin fluctuations and defining the lines of relatively sharp "pseudo- transitions" between them.
机译:在Bethe-Peierls近似中考虑了磁场中自旋冰磁石的短程模型的热力学。从[111],[100]和[011]场获得的结果与现有的蒙特卡洛模拟和一些实验相当吻合。在这种近似中,所有极尖锐的磁场引起的异常都通过温度和施加磁场的解析函数来描述。尽管没有真正的相变,但通过对HT平面上的熵和比热的分析,可以辨别具有自旋涨落特征的“伪相”,并在两者之间定义相对尖锐的“伪相变”线。他们。

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