Abstract
Recently, we observed a kagome-ice-like partial ferromagnetic order with coexisting fluctuation in a deformed pyrochlore structure . Here, we show that when lattice defects are present, the remaining fluctuating spins in this material further freeze at lower temperatures below after it initially freezes into the partial ferromagnetic order near . This low-temperature transition is glasslike requiring an extremely slow relaxation process in . Enhanced disorder in leads to a short-range order for the fluctuating spins. This result can be considered as an interesting analogy to the low-temperature anomaly in defect-containing pure and doped water ice, especially in the light of its relevance to the problem of residual entropy in ice-water or spin-ice transition.
- Received 2 August 2007
DOI:https://doi.org/10.1103/PhysRevB.77.024418
©2008 American Physical Society