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Low-temperature properties of the dilute dipolar magnet LiHo_xY_(1-x)F_4

机译:稀偶极磁体LiHo_xY_(1-x)F_4的低温特性

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摘要

We analyze recent experiments on the dilute rare-earth compound LiHo_xY_(1-x)F_4 in the context of an effective Ising dipolar model. Using a Monte Carlo method we calculate the low-temperature behavior of the specific heat and linear susceptibility and compare our results to measurements. In our model the susceptibility follows a Curie-Weiss law at high temperature, X ~1/(T-T_(cw)), with a Curie-Weiss temperature that scales with dilution, T_(cw) ~x, consistent with early experiments. We also find that the peak in the specific heat scales linearly with dilution, C_(max)(T)~x, in disagreement with recent experiments. This difference could be caused by the hyperfine interaction which is not included in our calculation. Experimental studies do not reach a consensus on the functional form of the susceptibility and specific heat, and in particular, we do not see reported scalings of the form X ~ T~(-0.75) and X-exp(-T/T_0). Furthermore, we calculate the ground-state magnetization as a function of dilution and re-examine the phase diagram around the critical dilution x_c =0.24 ±0.03. We find that the spin-glass susceptibility for the Ising model does not diverge below x_c, while some recent experiments give strong evidence for a stable spin-glass phase in LiHo_(0.167)Y_(0.833)F)4.
机译:我们在有效的伊辛偶极模型的背景下分析了稀稀土化合物LiHo_xY_(1-x)F_4的最新实验。使用蒙特卡洛方法,我们计算了比热和线性磁化率的低温行为,并将我们的结果与测量结果进行了比较。在我们的模型中,在高温下,磁化率遵循居里-魏斯定律X〜1 /(T-T_(cw)),居里-魏斯温度随稀释度成比例地变化,T_(cw)〜x,与早期实验一致。我们还发现,比热的峰值随稀释度C_(max)(T)〜x呈线性变化,这与最近的实验不一致。这种差异可能是由我们的计算中未包括的超精细相互作用引起的。实验研究尚未就磁化率和比热的功能形式达成共识,特别是,我们没有看到报道的X〜T〜(-0.75)和X-exp(-T / T_0)的缩放比例。此外,我们将基态磁化强度计算为稀释度的函数,然后重新检查临界稀释度x_c = 0.24±0.03附近的相图。我们发现,Ising模型的自旋玻璃磁化率在x_c以下没有差异,而最近的一些实验为LiHo_(0.167)Y_(0.833)F)4中稳定的自旋玻璃相提供了有力的证据。

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