Abstract
The magnetic and transport properties of pyrochlore have been studied with variation of the rare earth ( ). The change of the mean ionic radius of , which induces change of the lattice structure, determines the magnetic ground state (ferromagnetic or spin glass), and the magnetic phase boundary is correlated with the metal-insulator crossover. Furthermore, we found enhanced magnetoresistance and unusual residual anomalous Hall effect at low temperatures near the phase boundary, which can be attributed to the coexistence of both phases.
- Received 23 July 1999
DOI:https://doi.org/10.1103/PhysRevLett.84.1998
©2000 American Physical Society