Study of Magnetic and Dielectric Properties of Rare Earth Iron Garnets

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dc.contributor.author Aakansha
dc.date.accessioned 2020-10-13T11:11:36Z
dc.date.available 2020-10-13T11:11:36Z
dc.date.issued 2019
dc.identifier.other ROLL NO.146121022
dc.identifier.uri http://gyan.iitg.ernet.in/handle/123456789/1730
dc.description Supervisor: S. Ravi en_US
dc.description.abstract The current Ph.D. thesis presents the investigation and characterization of magnetic and dielectric properties of Y3Fe5O12 (YIG) and Gd3Fe5O12 (GIG) by substituting trivalent Sm and Bi at Y and Gd site, and Cr and Mn at Fe site respectively. The polycrystalline samples of the mentioned materials were synthesized by conventional solid-state reaction method. All the samples are found to be in single phase form as per the Rietveld refinement of XRD patterns using cubic space group Ia-3d. All samples exhibit ferrimagnetic (FIM) transition. However, GIG undergoes a magnetic compensation (Tcomp) behaviour near room temperature. Sm and Bi substitution enhances the FIM transition temperature (TC ) while the Cr and Mn substitution reduces the FIM TC. The increment (reduction) in bond angle strengthens (weakens) the superexchange interaction in (Fe3+-O2--Fe3+) networks, thereby increases (reduces) the FIM TC. Cr substitution in YIG reduces the FIM TC from 550 K to 494 K while Bi substitution in GIG enhances it from 560 K to 594 K, which is highest among all of the samples. Furthermore, an interesting negative magnetization is observed in Gd1Sm2Fe5O12 sample below Tcomp=70 K due to high magnetic anisotropy of Sm3+ ions. In addition to magnetic properties, these samples are also examined for dielectric properties using impedance spectroscopy. The impedance spectroscopy analysis were carried from the frequency variation data of real (Z') and imaginary (Z'') components of impedance. Further, the grains (G) and grain boundaries (GB) contributions were determined from Nyquist plots (Z'' vs Z'). These plots were explained based on an equivalent circuit having resistance, capacitance and constant phase element components arranged parallel to each other. From the analysis, both G and GB are found to contribute towards conduction process at lower temperature however, GB contribution is found to be dominant at higher temperature due to the long-range hopping of charge carriers. Cr substituted YIG samples show the increase in dielectric constant from 12 to 52 determined from analysis based on Havriliak‒Negami equations. Garnets exhibit centrosymmetric nature, which limits them from ferroelectricity. But in our case, Bi substitution at Gd site gives rise the presence of relaxor type ferroelectric behavior due to the inclusion of nano-polar region associated to the Bi3+ and Fe2+/Fe3+ ions. The Kohlrausch-Williams-Watts (KWW) function is used to explain the modulus spectra in Cr-substituted GIG compound and they exhibit relaxation peak associated to grains. All the samples possess magnetoelectric coupling in the vicinity of FIM TC. So, the presence of negative magnetization, relaxor ferroelectric behavior and magnetoelectric coupling in these samples may pave for exploration for memory storage and multiferroic applications. en_US
dc.language.iso en en_US
dc.relation.ispartofseries TH-2284;
dc.subject PHYSICS en_US
dc.title Study of Magnetic and Dielectric Properties of Rare Earth Iron Garnets en_US
dc.type Thesis en_US


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