arXiv · 1804.05401
Evidence for superferrimagnetic clusters and spin-glass transition involving 4f Dy3+ spins in h-DyMnO3: A new twist to 4f Re3+ spin ordering in hexagonal manganites
Abstract
The ferroelectric phase of the multiferroic hexagonal manganites (h-ReMnO3) has been reported to undergo a series of magnetic transitions involving long-range ordering/reorientation of 4fRe3+ and/or 3dMn3+ spins below room temperature. These transitions have attracted a lot of attention in recent years due to the geometrically frustrated nature of magnetic interactions. We have revisited these transitions in high quality single crystals of h-DyMnO3 using dc and ac susceptibility measurements as a function of temperature (T), magnetic field (H) and frequency (w) supplemented by specific heat measurements. Taking h-DyMnO3 as an example, we show that the Dy3+ spins below TN~68K are in a superferrimagnetic (SFIM) state whereas they undergo spin-glass (SG) transition below TDy3+~7K. Our observations demonstrate that neither the N\'eel transition at TN~68K nor the transition at TDy3+~7K is associated with long-range ordered states of Dy3+ spins as believed so far in the literature. The SG state of h-DyMnO3 is quite exotic as it occurs in an ordered compound purely due to geometrical frustration without any random disorder. Further, it shows an interesting crossover from de Almeida-Thouless type exponent (m=2/3) to Gabay-Toulouse type (m=2) with increasing field which cannot be explained in terms of the existing mean field theories of SG transition in Ising or Heisenberg systems but is expected for a vector X-Y SG system. Our observations call for a systematic reinvestigation of the nature of magnetic transitions involving Re3+ ions in other h-ReMnO3 also.
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P. Aravinth Kumar, Arun Kumar, Keshav Kumar, G. Anandha Babu, P. Vijayakumar, S. Ganesamoorthy, P. Ramasamy, Dhananjai Pandey. 2018-04-15. Evidence for superferrimagnetic clusters and spin-glass transition involving 4f Dy3+ spins in h-DyMnO3: A new twist to 4f Re3+ spin ordering in hexagonal manganites. https://arxiv.org/abs/1804.05401
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