2006
DOI: 10.1016/j.crhy.2005.11.010
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The ruthenocuprates: natural superconductor–ferromagnet multilayers

Abstract: The recently discovered ruthenocuprates have attracted great interest because of the microscopic coexistence of superconducting and ferromagnetic order. Typically, these materials become magnetically ordered at temperatures around 125-145 K and superconductivity sets in between 15 and 50 K. While superconductivity arises in the CuO2 layers the RuO2 layers in between order magnetically. In this paper we summarize some of the crystallographic, magnetic and superconducting properties of the ruthenocuprates, as ob… Show more

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Cited by 39 publications
(38 citation statements)
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References 96 publications
(182 reference statements)
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“…21 However, as mentioned in Sect. I, there were many different interpretations 2,14-16 reviewed in Ref.…”
Section: Magnetization Measurementsmentioning
confidence: 95%
“…21 However, as mentioned in Sect. I, there were many different interpretations 2,14-16 reviewed in Ref.…”
Section: Magnetization Measurementsmentioning
confidence: 95%
“…RuSr 2 GdCu 2 O 8 (Ru1212) and related compounds with alternating RuO 2 and CuO 2 layers have attracted tremendous scientific interest in recent years, mainly due to the microscopic coexistence of long-range magnetic order and superconductivity [1][2][3]. With a magnetic ordering temperature T N ¼ 100-150 K and a superconducting transition temperature of $15-50 K, Ru1212 exhibits not only the highest magnetic transition temperature among all magnetic superconductors, but also the broadest coexistence range of magnetic order and superconductivity.…”
mentioning
confidence: 99%
“…Despite the intensive investigation of ruthenatecuprates in the last ten years, a lot of questions about the nature of magnetic order and superconductivity, in particular their coexistence, are still unanswered [1]. It is well established that in RuSr 2 RCu 2 O 8 (Ru1212R, R = Eu, Gd, Y) compounds the magnetic ordering of ruthenium sublattice occurs at about 130 K. The ordering is predominantly antiferromagnetic (AFM) with an easy axis perpendicular to the layers and with a weak ferromagnetic (FM) component parallel to the layers.…”
Section: Introductionmentioning
confidence: 99%