Hindmarch A T, Hickey B J
Department of Physics & Astronomy, University of Leeds, Leeds, LS2 9JT United Kingdom.
Phys Rev Lett. 2003 Sep 12;91(11):116601. doi: 10.1103/PhysRevLett.91.116601. Epub 2003 Sep 9.
We show that the ferromagnetic heavy rare-earth (RE) metals show a transport spin polarization at the Fermi level in the majority spin, whereas in ferromagnetic light rare earths it is in the minority spin. The sign of the polarization is in agreement with what is expected due to the Ruderman-Kittel-Kasuya-Yosida (RKKY) coupling formalism. We show that magnetotransport measurements on magnetic multilayer samples containing magnetic REs provide a unique opportunity to verify the RKKY coupling scheme in pure rare-earth metals, allowing us to probe both the sign and temperature dependence of the spin-density oscillation.
我们表明,铁磁重稀土(RE)金属在费米能级处的多数自旋中呈现出输运自旋极化,而在铁磁轻稀土中则是在少数自旋中呈现。这种极化的符号与基于鲁德曼 - 基特尔 - 卡苏亚 - 约西达(RKKY)耦合形式理论所预期的一致。我们还表明,对含有磁性稀土的磁性多层样品进行磁输运测量,为验证纯稀土金属中的RKKY耦合方案提供了独特的机会,使我们能够探究自旋密度振荡的符号和温度依赖性。