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arXiv 0802.1664cond-mat.str-elcond-mat.mtrl-sci
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掺杂锰氧化物电阻率峰起源处的双流体行为

Two-Fluid Behaviour at the Origin of the Resistivity Peak in Doped Manganites

D. I. Golosov, N. Ossi, A. Frydman, I. Felner, I. Nowik, M. I. Tsindlekht, Y. M. Mukovskii

摘要:

本文报道了高质量巨磁阻锰氧化物单晶样品La_{0.7} Ca_{0.3} Mn O_3和Pr_{0.7} Sr_{0.3} Mn O_3的一系列磁性和输运测量结果。1%Fe掺杂允许穆斯堡尔谱研究,其显示(i)铁磁相内的不寻常的谱线加宽和(ii)铁磁和顺磁贡献在居里点T_C附近的区域T_1<T<T_2中共存。在Pr_{0.7} Sr_{0.3} Mn O_3的情况下,电阻率峰值出现在相当高的温度下,T_{MI} >T_2。这表明,相分离成金属(铁磁)和绝缘(顺磁)相一般不能负责的电阻率峰值(并因此为相关的庞磁阻)。我们的结果可以理解现象学内的双流体的方法,这也允许T_C和T_{MI}之间的差异。我们的数据确实意味着锰氧化物的磁性和输运性质是密切相关的,在T_C和T_{MI}的两个转变可以被看作是不同的现象。

英文摘要:

We report a series of magnetic and transport measurements on high-quality single crystal samples of colossal magnetoresistive manganites, La_{0.7} Ca_{0.3} Mn O_3 and Pr_{0.7} Sr_{0.3} Mn O_3. 1 % Fe doping allows a Moessbauer spectroscopy study, which shows (i) unusual line broadening within the ferromagnetic phase and (ii) a coexistence of ferro- and paramagnetic contributions in a region, T_1<T<T_2, around the Curie point T_C. In the case of Pr_{0.7} Sr_{0.3} Mn O_3, the resistivity peak occurs at a considerably higher temperature, T_{MI}>T_2. This shows that phase separation into metallic (ferromagnetic) and insulating (paramagnetic) phases cannot be generally responsible for the resistivity peak (and hence for the associated colossal magnetoresistance). Our results can be understood phenomenologically within the two-fluid approach, which also allows for a difference between T_C and T_{MI}. Our data indeed imply that while magnetic and transport properties of the manganites are closely interrelated, the two transitions at T_C and T_{MI} can be viewed as distinct phenomena.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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