Abstract
In this work, La0.75Ca0.25FeO3−δ perovskite sample was prepared by the coprecipitation method. The nanoparticle was found to crystallize in the orthorhombic (Pbnm) phase as confirmed by X-ray diffraction (XRD) and transmission electron microscopic (TEM). The oxygen non-stoichiometry (δ) and magnetic states of iron ions (three magnetic sextets and non-magnetic doublet) were investigated by Mössbauer spectroscopy at room temperature (RT). The shape of the magnetic hysteresis loop of the sample reveals the existence of a weak ferromagnetism at RT. The magnetization vs. temperature curves, measured in the 9 to 200 K range, showed that the sample exhibits two magnetic-phase transition temperatures at 29 K (Tg) and 120 K (TCO). The magnetization isotherms, M (H), around these magnetic-phase transition temperatures for the sample are analyzed.
| Original language | English |
|---|---|
| Pages (from-to) | 1346-1359 |
| Number of pages | 14 |
| Journal | Philosophical Magazine |
| Volume | 97 |
| Issue number | 16 |
| DOIs | |
| State | Published - 3 Jun 2017 |
Bibliographical note
Publisher Copyright:© 2017 Informa UK Limited, trading as Taylor & Francis Group.
Keywords
- Mössbauer spectroscopy
- Perovskite
- X-ray diffraction
- magnetic-phase transitions
ASJC Scopus subject areas
- Condensed Matter Physics