Abstract
An incommensurate composite phase with a monoclinic host-guest structure, designated , is found between the previously known and phases, and an incommensurate to incommensurate transition between phases II and IV is described. The monoclinic phase is observed on both pressure increase between 8.2 and and on pressure decrease between 8.0 and . The full structure of , including a determination of the structural modulations of the host and guest components, is reported from x-ray powder diffraction data. The high-pressure phase of arsenic, , is shown to have the same monoclinic composite structure.
- Received 19 December 2003
DOI:https://doi.org/10.1103/PhysRevB.70.184119
©2004 American Physical Society