Ice Ic ( Ice one cubic)
- can be formed by condensation of water vapour at reduced pressure well below -80 °C
- is metastable with respect to Ice Ih (approx. + 50 J/mol)
- it seems to be very difficult to grow large phase-pure Ic ice crystals; they contain, to a certain extent stacking-disordered or hexagonal ice
Structural features:
- like hexagonal ice cubic ice is a proton-disordered phase
- every water molecule is involved in 4 H-bonds (2 acceptors, 2 donors)
- tetrahedrally coordinated
- O-D bond length approx. 101 pm
- D …. O-D distance approx. 174 pm
- O … O distance approx. 275 pm
- 6-membered rings (exclusively chair conformation)
- sometimes also called “cristobalite ice” because the oxygen atoms occupy the Si analogeous positions in the SiO2 phase cristobalite
- it would be also justified to call it diamond-like ice 🙂
- Space group Fd-3m
- a = b = c = 6.3510 Å
- α = β = γ = 90°
Here, you can download the CIF.
[Atomic structure figures created with VESTA:
K. Momma and F. Izumi, “VESTA 3 for three-dimensional visualization of crystal, volumetric and morphology data,” J. Appl. Crystallogr., 44, 1272-1276 (2011).]