Abstract
The latent heat associated with the orbital order-disorder transition at is found to depend significantly on the average particle size of . It rises slowly with the decrease in down to and then jumps by more than an order of magnitude in between and . Finally, falls sharply to zero at a critical particle size . The transition temperature also exhibits an almost similar trend of variation with the particle size, near and below, even though the extent of variation is relatively small. The zero-field-cooled (ZFC) and field-cooled (FC) magnetization versus temperature study over a temperature range reveals that the antiferromagnetic transition temperature decreases with while the temperature range, over which the ZFC and FC data diverge, increases with the drop in . The FC magnetization also is found to increase sharply with the drop in particle size. A conjecture of nonmonotonic variation in orbital domain structure with decrease in particle size—from smaller domains with large number of boundaries to larger domains with small number of boundaries due to lesser lattice defects and, finally, down to even finer domain structures with higher degree of metastability—along with increase in surface area in core-shell structure, could possibly rationalize the observed versus and versus patterns. Transmission electron microscopy data provide evidence for presence of core-shell structure as well as for increase in lattice defects in finer particles.
- Received 21 November 2005
DOI:https://doi.org/10.1103/PhysRevB.74.014410
©2006 American Physical Society