Please use this identifier to cite or link to this item:
Title: Effects of 18O isotope substitution in multiferroic RMnO3 (R=Tb, Dy)
Authors: Graham, PJ
Narayanan, N
Reynolds, NM
Li, F
Rovillain, P
Bartkowiak, M
Hester, JR
Kimpton, JA
Yethiraj, M
Pomjakushina, E
Conder, K
Kenzelmann, M
McIntyre, GJ
Hutchison, WD
Ulrich, C
Keywords: Coupling
Crystal structure
Electric properties
Magnetic fields
Maganese oxides
Memory devices
Neutron diffraction
Oxygen isotopes
Phase transformations
Raman spectroscopy
Issue Date: 2-Feb-2015
Publisher: Australian Institute of Physics
Citation: Graham, P. J., Narayanan, N., Reynolds, N., Li, F., Rovillain, P., Bartkowiak, M., Hester, J., Kimpton, J., Yethiraj, M., Pomjakushina, E., Conder, K., Kenzelmann, M., McIntyre, G., Hutchison, W., D., & Ulrich, C. (2015). Effects of 18O isotope substitution in multiferroic RMnO3 (R=Tb, Dy). Paper presented at the 39th Annual Condensed Matter and Materials Meeting, Charles Sturt University, Wagga Wagga, NSW, 3 February 2015 - 6 February 2015, (pp. 57). Retrieved from:
Abstract: Multiferroic materials demonstrate desirable attributes for next-generation multifunctional devices as they exhibit coexisting ferroelectric and magnetic orders. In type-II multiferroics, coupling exists that allows ferroelectricity to be manipulated via magnetic order and vice versa, offering potential in high-density information storage and sensor applications. Despite extensive investigations into the subject, questions of the physics of magnetoelectric coupling in multiferroics remain, and competing theories propose different mechanisms. The aim of this investigation was to study changes in the statics and dynamics of structural, ferroelectric and magnetic orders with oxygen-18 isotope substitution to shine light into the coupling mechanism in multiferroic RMnO3 (R=Tb, Dy) systems. We have performed Raman spectroscopy on 16O and 18O-substituted TbMnO3 single crystals. Oxygen-18 isotope substitution reduces all phonon frequencies significantly. However, specific heat measurements determine no changes in Mn3+ (28 and 41 K) magnetic phase transition temperatures. Pronounced anomalies in peak position and linewidth at the magnetic and ferroelectric phase transitions are seen. While the anomalies at the sinusoidal magnetic phase transition (41 K) are in accordance to the theory of spin-phonon coupling, further deviations develop upon entering the ferroelectric phase (28 K). Furthermore, neutron diffraction measurements on 16O and 18O-substituted DyMnO3 powders show structural deviations at the ferroelectric phase transition (17 K) in the order of 100 fm. These results indicate that the structure is actively involved in the emergence of ferroelectricity in these materials.
ISBN: 978-0-646-96433-1
Appears in Collections:Conference Publications

Files in This Item:
File Description SizeFormat 
Wagga2015_10_Handbook(1).pdf39.53 MBAdobe PDFThumbnail

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.