Sakakibara T, Tayama T, Hiroi Z, Matsuhira K, Takagi S
Institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan.
Phys Rev Lett. 2003 May 23;90(20):207205. doi: 10.1103/PhysRevLett.90.207205.
Low temperature magnetization measurements on the pyrochlore spin ice compound Dy2Ti2O7 reveal that the ice-rule breaking spin flip, appearing at H approximately 0.9 T applied parallel to the [111] direction, turns into a novel first-order transition for T<0.36 K which is most probably of a liquid-gas type. T-linear variation of the critical field observed down to 0.03 K suggests the unusual situation that the entropy release across the transition remains finite [approximately 0.5 (J/K) x mol-Dy] as T-->0, in accordance with a breaking of the macroscopic degeneracy in the intermediate "kagomé ice" state.
对烧绿石自旋冰化合物Dy2Ti2O7进行的低温磁化测量表明,在平行于[111]方向施加的约0.9 T磁场下出现的违反冰规则的自旋翻转,在T < 0.36 K时转变为一种新型的一级相变,很可能是液-气类型。在低至0.03 K时观察到的临界场的T线性变化表明了一种不寻常的情况,即随着T→0,跨越相变的熵释放保持有限[约0.5 (J/K)×mol-Dy],这与中间“ kagomé冰”状态下宏观简并性的破坏一致。