Praseodymium Calcium Manganites : Magnetism Across Length Scales

dc.contributorMatemaattis-luonnontieteellinen tiedekunta / Faculty of Mathematics and Natural Sciences, Department of Physics and Astronomy-
dc.contributor.authorTikkanen, Jussi
dc.contributor.departmentfi=Fysiikan ja tähtitieteen laitos|en=Department of Physics and Astronomy|
dc.contributor.facultyfi=Matemaattis-luonnontieteellinen tiedekunta|en=Faculty of Mathematics and Natural Sciences|-
dc.date.accessioned2017-06-09T09:48:10Z
dc.date.available2017-06-09T09:48:10Z
dc.date.issued2017-06-30
dc.description.abstractIn this work, the methods of experimental and computational material physics are employed to describe and explain the magnetic phase diagram of Pr1−xCaxMnO3, a particular family of perovskite-structured manganites (here-after PCMO) perhaps most famous for its prominent colossal magnetoresistivity effect. After introducing the basic structural and magnetic properties of perovskite manganites and finally the macroscopic magnetic phase diagram of PCMO, the microscopic mechanisms at the origin of the directly observable macroscopic phases of PCMO are identified and modeled. The experimental research was largely based on ceramic samples synthesized by the traditional solid state method. The highly crystalline samples were readily characterized by diffractometric methods, including x-ray and neutron diffraction assisted by Rietveld refinement, and bulk magnetometry down to the liquid helium temperature. Thus, experimental correlations between the structural and magnetic properties of PCMO could be established. Structural problems only arose at the highest of Ca concentrations, at x ≥ 0.8, where a structural phase separation and a thermodynamic preference for severe oxygen understoichiometry were verified. At x ≤ 0.8, a consistent description of the magnetic phase diagram was achieved based on a microscopic dynamic equilibrium between only two magnetic phases, significantly extending the range of applicability of such a framework for PCMO. The phase equilibrium was characterized via several distinct observations of structural transitions and exotic magnetization dynamics, and finally modeled by Monte Carlo simulations capable of reproducing the magnetic hysteresis of PCMO, including the metamagnetic transition related to the colossal magnetoresistance effect. As a natural byproduct of analyzing the magnetic transitions, entropy-based estimates for the magnetocaloric applicability of PCMO were also obtained. The estimated refrigerant capacities placed the 100 K performance of PCMO on par with the room temperature figures of some of the best Gd-based magnetocaloric alloys.-
dc.description.accessibilityfeatureei tietoa saavutettavuudesta
dc.description.notificationSiirretty Doriasta
dc.format.contentfulltext
dc.identifierISBN 978-951-29-6873-2-
dc.identifier.olddbid152825
dc.identifier.oldhandle10024/136367
dc.identifier.urihttps://www.utupub.fi/handle/11111/28312
dc.identifier.urnURN:ISBN:978-951-29-6873-2-
dc.language.isoeng-
dc.publisherfi=Turun yliopisto|en=University of Turku|
dc.publisherAnnales Universitatis Turkuensis A I 562-
dc.relation.ispartofseriesTurun yliopiston julkaisuja. Sarja AI, Chemica - Physica – Mathematica
dc.relation.issn2343-3175
dc.relation.numberinseries562-
dc.source.identifierhttps://www.utupub.fi/handle/10024/136367
dc.titlePraseodymium Calcium Manganites : Magnetism Across Length Scales-
dc.type.ontasotfi=Artikkeliväitöskirja|en=Doctoral dissertation (article-based)|

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