Abstract
The crystallographic and magnetic microstructure of magnetite (Fe 304) below the Verwey transition (∼120K) is studied using transmission electron microscopy. The low temperature phase is found to have a monoclinic C-centered lattice with a c-glide plane perpendicular to the A-axis, which allows twin-related crystal orientations to be distinguished. Off-axis electron holography and Lorentz electron microscopy are used to show that magnetic domains present at room temperature become subdivided into sub-micron-sized magnetic domains below the Verwey transition, with the magnetization direction in each magnetic domain oriented along the monoclinic [001] axis. The nature of the interactions between the magnetic domain walls and the ferroelastic twin walls is investigated. Cooling and warming cycles through the transition temperature are used to show that a memory effect is likely to exist between the magnetic states that form above and below the transition. Our results suggest that ferroelastic twin walls have a strong influence on the low temperature magnetic properties of magnetite.
Original language | English |
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Pages (from-to) | 67-87 |
Number of pages | 21 |
Journal | Phase Transitions |
Volume | 86 |
Issue number | 1 |
DOIs | |
Publication status | Published - 2013 Jan |
Externally published | Yes |
Keywords
- Ferroelastic twins
- Low temperature magnetic properties
- Magnetite
- Multiferroics
- Transmission electron microscopy
- Verwey transition
ASJC Scopus subject areas
- Instrumentation
- Materials Science(all)