Cs4O6 adopts two distinct crystal structures
at ambient pressure. At temperatures below ∼200 K, its ground
state structure is tetragonal, incorporating two symmetry-distinct
dioxygen anions, diamagnetic peroxide, O2
2–, and paramagnetic superoxide, O2
–,
units in a 1:2 ratio, consistent with the presence of charge and orbital
order. At high temperatures, its ground state structure is cubic,
comprising symmetry-equivalent dioxygen units with an average oxidation
state of −4/3, consistent with the adoption
of a charge-disordered state. The pressure dependence of the structure
of solid Cs4O6 at 300 K and at 13.4 K was followed
up to ∼12 GPa by synchrotron X-ray powder diffraction. When
a pressure of ∼2 GPa is reached at ambient temperature, an
incomplete phase transition that is accompanied by a significant volume
reduction (∼2%) to a more densely packed highly anisotropic
tetragonal structure, isostructural with the low-temperature ambient-pressure
phase of Cs4O6, is encountered. A complete transformation
of the cubic (charge-disordered) to the tetragonal (charge-ordered)
phase of Cs4O6 is achieved when the hydrostatic
pressure exceeds 6 GPa. In contrast, the pressure response of the
Cs4O6 cubic/tetragonal phase assemblage at 13.4
K is distinctly different with the cubic and tetragonal phases coexisting
over the entire pressure range (to ∼12 GPa) accessed in the
present experiments and with only a small fraction of the cubic phase
converting to tetragonal. Pressure turns out to be an inefficient
stimulus to drive the charge disorder–order transition in Cs4O6 at cryogenic temperatures, presumably due to
the high activation barriers (much larger than the thermal energy
at 13.4 K) associated with the severe steric hindrance for a rotation
of the molecular oxygen units necessitated in the course of the structural
transformation.