Role of external and internal perturbations on ferromagnetic phase transitions in manganites: Existence of tricritical points

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Abstract

A phenomenological mean-field theory
is presented to describe the role of external magnetic field,
pressure and chemical substitution on the nature of ferromagnetic (FM) to paramagnetic (PM) phase transition in manganites. The application of external field (or pressure) shifts the transition, leading to a field (or pressure) dependent phase boundary along which a tricritical point is shown to exist where a first-order FM-PM transition becomes second-order. We show that the effect of chemical substitution on the FM transition is analogous to that of external perturbations (magnetic field and pressure); this includes the existence of a tricritical point at which the order of transition changes. Our theoretical predictions satisfactorily explain the nature of FM-PM transition, observed in several systems. The modeling hypothesis has been critically verified from our experimental data from a wide range of colossal magnetoresistive manganite single crystals like Sm$_{0.52}$Sr$_{0.48}$MnO$_3$. The theoretical model prediction of a tricritical point has been validated in this experiment which provides a major ramification of
the strength of the model proposed.

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  • Role of external and internal perturbations on ferromagnetic phase transitions

    Rights statement: This is an author-created, un-copyedited version of an article accepted for publication/published in [insert name of journal]. IOP Publishing Ltd is not responsible for any errors or omissions in this version of the manuscript or any version derived from it. The Version of Record is available online at https://doi.org/10.1088/1361-648X/aacb3a

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Original languageEnglish
JournalJournal of Physics: Condensed Matter
Early online date8 Jun 2018
DOIs
StateE-pub ahead of print - 8 Jun 2018

Bibliographic note

This is an author-created, un-copyedited version of an article accepted for publication/published in [insert name of journal]. IOP Publishing Ltd is not responsible for any errors or omissions in this version of the manuscript or any version derived from it. The Version of Record is available online at https://doi.org/10.1088/1361-648X/aacb3a

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