2017
DOI: 10.1016/j.jmmm.2017.07.015
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Critical phenomena in a mixed spin-3/2 and spin-5/2 Ising ferro-ferrimagnetic system in a longitudinal magnetic field

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Cited by 13 publications
(5 citation statements)
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“…This phenomenon does not occur in F systems. [ 56,84 ] The existence of these metastable states with very long lifetimes (larger than our MC runs) is not uncommon in systems with several competing magnetic orderings, with complicated ground state phase diagrams, and there is experimental evidence of their existence. [ 85,86 ] When T<Tk the AF ordering prevails, independently of the external field, for T>Tk the external field dominates such that the total magnetization decreases toward its saturation value where all the spins are parallel to the field.…”
Section: Resultsmentioning
confidence: 99%
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“…This phenomenon does not occur in F systems. [ 56,84 ] The existence of these metastable states with very long lifetimes (larger than our MC runs) is not uncommon in systems with several competing magnetic orderings, with complicated ground state phase diagrams, and there is experimental evidence of their existence. [ 85,86 ] When T<Tk the AF ordering prevails, independently of the external field, for T>Tk the external field dominates such that the total magnetization decreases toward its saturation value where all the spins are parallel to the field.…”
Section: Resultsmentioning
confidence: 99%
“…MC computational techniques have proven to be efficient for the analysis of Ising‐type magnetic models. [ 54–56 ]…”
Section: Model and Simulation Methodsmentioning
confidence: 99%
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“…En el caso que nos compete estudiaremos un ferrimagneto tipo Ising mixto de espines 𝑆 = 1 y 𝜎 = 2 estructurado en una red cuadrada. Cabe destacar que los modelos de Ising mixtos han probado ser de gran utilidad en la caracterización magnética de los complejos materiales magnéticos (De La Espriella, 2016;Žukovič and Bobák, 2016; Karimou and Bati, 2021), dado que se han obtenido interesantes resultados acerca de fenómenos críticos como comportamientos reentrantes, doblemente reentrantes y transiciones discontinuas (Magoussi et al, 2013;Temizer et al, 2016;De La Espriella et al, 2017), entre otros, en diversas redes cristalinas entre los que se destacan óxidos ferrimagnéticos amorfos con iones de Fe 3+ (Htoutou et al, 2004).…”
Section: Introductionunclassified