In situ neutron diffraction experiments show that at pressures above 2
kilobars, cubic zirconium tungstate (ZrW2O8) undergoes a quenchable p
hase transition to an orthorhombic phase, the structure of which has b
een solved from powder diffraction data. This phase transition can be
reversed by heating at 393 kelvin and 1 atmosphere and involves the mi
gration of oxygen atoms in the lattice. The high-pressure phase shows
negative thermal expansion from 20 to 300 kelvin. The relative thermal
expansion and compressibilities of the cubic and orthorhombic forms c
an be explained in terms of the ''cross-bracing'' between polyhedra th
at occurs as a result of the phase transition.