Abstract
Structural phase transitions of high-stage graphite intercalation compounds (GIC’s) have been investigated by using specific heat, x-ray (00L) and (HK0) diffraction, electron diffraction, and neutron (HKL) diffraction techniques. Each intercalate layer is uncorrelated with respect to the other intercalate layers but is modulated by the graphite layers. The stage-3 GIC undergoes a structural phase transition at =480 K, where the specific heat shows a λ-type anomaly and the c-axis repeat distance exhibits an abrupt increase as temperature is increased. The intercalate layer consists of the orthorhombic phase and the hexagonal phase. The orthorhombic phase forms a plane body-centered rectangular lattice with a=6.21±0.02 Å and b=17.93±0.02 Å at room temperature. The rotation angle between the a axis of the rectangular lattice and the graphite 〈100〉 direction of real space is θ=30°+Ω, with Ω=±8.1° below , and gradually changes to θ=30° well above . An explanation of the phase transition at is presented in terms of a rectangular superlattice that is commensurate with the graphite lattice.
- Received 31 October 1990
DOI:https://doi.org/10.1103/PhysRevB.43.5805
©1991 American Physical Society