Abstract
graphite bi-intercalation compounds (GBIC’s) with the stacking sequence -G--G--G- along the c axis have been prepared by a method of sequential intercalation. The intraplanar exchange interaction in layers is ferromagnetic, while the intraplanar exchange interaction in layers is antiferromagnetic. The magnetic properties of GBIC’s have been studied by using dc and ac magnetic susceptibility, and low- and high-field SQUID magnetization measurements. The layer undergoes a magnetic phase transition at the critical temperature which changes from 19.48 K at c=0 to 9.10 K at c=1. A cluster glass phase appears below where the spin directions of ferromagnetic clusters are frozen because of frustrated interisland interactions. Due to the intervening layer the critical behavior of - GBIC’s at is three dimensional rather than two dimensional.
Below (≊4 K) the cluster glass phase may coexist with an antiferromagnetic long-range order occurring in the layers. The effect of antiferromagnetic interplanar interaction between the layer and the layer is clearly seen in the magnetization of - GBIC’s. The nature of the coexisting phase is complicated by the spin frustration effect arising from the competition between the interplanar interaction between and layers and the antiferromagnetic intraplanar interaction in the layer.
- Received 20 June 1994
DOI:https://doi.org/10.1103/PhysRevB.50.12568
©1994 American Physical Society