1. Structural and magnetic properties of Ca3Mn2-xRux O7 (0<x≤0.9)
- Author
-
Blasco, Javier, Rodríguez-Velamazán, J. A., García Muñoz, Josep Lluís, Cuartero, Vera, Lafuerza, Sara, Subías, G., Ministerio de Ciencia, Innovación y Universidades (España), European Commission, Diputación General de Aragón, Agencia Estatal de Investigación (España), Ministerio de Economía y Competitividad (España), Blasco, Javier, and Cuartero, Vera
- Subjects
Magnetic phase transitions ,Ruthenates ,Manganites ,Crystal symmetry - Abstract
We here report on the study of the crystallographic and magnetic properties of layered perovskites Ca3Mn2-xRuxO7 (x≤0.9). We observe a solid solution between Mn and Ru atoms in the whole series and all samples present the same orthorhombic structure independently of the Ru content. Different magnetic structures, depending on the Ru content in the sample, have been determined using neutron powder diffraction. For low Ru doping (x≤0.1), there is a dominant G-type antiferromagnetic ordering in the perovskite bilayers but, differently from undoped Ca3Mn2O7, the magnetic moments are located on the ab plane. For higher Ru concentration (x≥0.3), the predominant G-type ordering is preserved along the y axis while an A-type component is developed along the x axis and its intensity increases as Ru content does. This component is characterized by a ferromagnetic ordering in the a direction of one of the Mn(Ru)O6 layers, coupled antiferromagnetically with the neighbor Mn(Ru)O6 layer within the same bilayer. The study of the macroscopic magnetic properties shows that ferromagneticlike correlations are enhanced with increasing Ru content as deduced from the shift to higher temperature of the onset of the magnetic transition temperature. The magnetic transitions take place in two steps. At higher temperatures (140-200 K), short-range magnetic correlations are established. Tiny spontaneous magnetization is observed in the hysteresis loops with small coercive field. At TN≈115-125K, long-range antiferromagnetic ordering is developed. The ferromagnetic component remains with a strong increase of coercivity. We discuss in the paper the possible origins of this ferromagnetic contribution., The authors would like to acknowledge the use of Servicio General de Apoyo a la Investigacion from Universidad de Zaragoza. For financial support, we thank the Spanish Ministerio de Economia y Competitividad [Projects No. RTI2018098537-B-C22 and No. RTI2018-098537-B-C21, cofunded by ERDF from EU, the "Severo Ochoa" Programme (FUNFUTURE (CEX2019-000917) and Diputacion General de Aragon (Project No. E12-17R, RASMIA). We thank the ILL for the beamtime allocation under Experiment No. 5-31-2788., With funding from the Spanish government through the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000917-S).
- Published
- 2022