Second order magnetic phase transition and scaling analysis in iron doped manganite La0.7Ca0.3Mn1−xFexO3 compounds
Creators
- 1. Department of Applied Physics and Institute of Natural Sciences, Kyung Hee University, Yong-in 446-701 (Korea, Republic of)
- 2. Physics Education, Syarif Hidayatullah State Islamic University, Jakarta 15412 (Indonesia)
- 3. Department of Electrical Engineering, University of Sultan Ageng Tirtayasa, Banten 42435 (Indonesia)
- 4. Department of Mechanical Engineering, Mercu Buana University, Jakarta-Barat, Jakarta 11650 (Indonesia)
- 5. Department of Mechanical Engineering, State Polytechnic of Malang, East Java 65100 (Indonesia)
- 6. Institute of Electronic Materials, University of Wollongong, Wollongong NSW 2522 (Australia)
- 7. PSTBM-BATAN, Kawasan Puspiptek Serpong, Tangerang Selatan, Banten 15314 (Indonesia)
Description
We investigated magnetic properties of La0.7Ca0.3Mn1−xFexO3 (x=0.09 and 0.11) compounds in terms of isothermal magnetization analysis and scaling behavior with various critical exponents. From the Landau theory of magnetic phase transition, we found that the paramagnetic to ferromagnetic phase transition in La0.7Ca0.3Mn1−xFexO3 (x=0.09 and 0.11) compounds is the type of second order magnetic transition (SOMT), which contrary to the first order magnetic transition (FOMT) for low Fe-doped compounds (x<0.09) in previous reports. When we investigate the critical behavior of the compounds near T=Tc by the modified Arrott plot, Kouvel–Fisher plots, and critical isothermal analysis, the estimated critical exponents β, γ, and δ are in between the theoretically predicted values for three-dimensional Heisenberg and mean-field interaction models. It is noteworthy that the scaling relations are obeyed in terms of renormalization magnetization m=ε−βM(H,ε) and renormalized field h=|ε|β+γH. Temperature-dependent effective exponents βeff and γeff correspond to the ones of disordered ferromagnets. It is shown that the magnetic state of the compounds is not fully described by the conventional localized-spin interaction model because the ferromagnetic interaction has itinerant character by increasing Fe-doping concentration. - Highlights: • The ferromagnetic phase transition is of second order in La0.7Ca0.3Mn1−xFexO3. • The critical exponents are in between the 3D Heisenberg and mean-field models. • The ferromagnetic interaction becomes more itinerant by Fe-doping
Availability note (English)
Available from http://dx.doi.org/10.1016/j.jmmm.2015.07.033Additional details
Identifiers
- DOI
- 10.1016/j.jmmm.2015.07.033;
- PII
- S0304-8853(15)30344-9;
Publishing Information
- Journal Title
- Journal of Magnetism and Magnetic Materials
- Journal Volume
- 395
- Journal Page Range
- p. 41-47
- ISSN
- 0304-8853
- CODEN
- JMMMDC
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 47038889
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- CALCIUM COMPOUNDS; CONCENTRATION RATIO; DOPED MATERIALS; FERROMAGNETIC MATERIALS; FERROMAGNETISM; HEISENBERG MODEL; IRON COMPOUNDS; LANTHANUM COMPOUNDS; MAGNETIC PROPERTIES; MAGNETIZATION; MANGANATES; MEAN-FIELD THEORY; PARAMAGNETISM; PEROVSKITE; PHASE TRANSFORMATIONS; RENORMALIZATION; SPIN; TEMPERATURE DEPENDENCE; THREE-DIMENSIONAL LATTICES
- Descriptors DEC
- ALKALINE EARTH METAL COMPOUNDS; ANGULAR MOMENTUM; CRYSTAL LATTICES; CRYSTAL MODELS; CRYSTAL STRUCTURE; DIMENSIONLESS NUMBERS; MAGNETIC MATERIALS; MAGNETISM; MANGANESE COMPOUNDS; MATERIALS; MATHEMATICAL MODELS; MINERALS; OXIDE MINERALS; OXYGEN COMPOUNDS; PARTICLE PROPERTIES; PEROVSKITES; PHYSICAL PROPERTIES; RARE EARTH COMPOUNDS; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2015 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.