Rietveld analysis of synchrotron X-ray powder diffraction data for the silica mineral moganite from 100 K to 1354 K has revealed a reversible phase transition from space group 12/a to Imab at approximately 570 K. The thermal expansion behavior of the lattice parameters alters sharply at the transition point, and the monoclinic β angle decreases to 90°. The displacive transition from α- to β- moganite is effected by the rotation of apparently rigid tetrahedra about the  axis, and the linear temperature dependence of the volume strain and of the non-symmetry-breaking e11 and e22 strains indicates that the character of the transition is second-order. The continuous increase in the b axis over the entire temperature range reveals a concomitant rotation of tetrahedra about  that does not affect the overall symmetry. In addition, we present a refinement without structural constraints for α-moganite at room temperature using time-of-flight neutron diffraction data.
|Original language||English (US)|
|Number of pages||9|
|State||Published - Jan 1 2001|
All Science Journal Classification (ASJC) codes
- Geochemistry and Petrology