Abstract
High-frequency magnetic resonance measurements were employed to investigate the low-temperature antiferromagnetic ground state of the fulleride. The frequency and temperature dependence of the intensity, linewidth, and center of the resonance signal detected below are characteristic of antiferromagnetic resonance (AFMR). The AFMR intensity is consistent with an ordered magnetic moment of , while the narrowing of the AFMR signal with increasing resonance frequency can be modeled with a spin-flop field of and a -factor anisotropy of . We stress that the spin-flop field is reduced compared to the ammoniated analog on the account of reduced exchange interactions. Differences in the level of the anisotropic expansion between and cointercalated fullerides are likely to be responsible for the differences in the electronic structure between the two systems and ultimately may account for the reduced Néel temperature in .
- Received 7 May 2007
DOI:https://doi.org/10.1103/PhysRevB.77.035104
©2008 American Physical Society