Tag Archives: Ice

Ice IV – a remarkable self-interpenetrating structure

Ice IV (Ice four)

  • metastable in the phase space between Ice III, Ice V and Ice VI (see orange circle in the Figure above)
  • may be formed from high-density amorphous ice by slow heating from 145 K and a constant pressure of 8 kbar
  • calc. density at 110 K and 1 bar = 1.27 g/cm3

Structural features

  • proton-disordered phase
  • all water molecules are hydrogen-bonded to four others, two as donor and two as acceptor
  • exclusively 6-membered rings (two types, one almost flat, the other more puckered)
  • the most striking structural feature is that Ice IV builds a self-interpenetrating structure, but this does not consists of two independent networks but of only one net: two water molecules (shown in blue in the following Figure) bonded by H-bonds are oriented perpendicular and are running through the center of the almost flat 6-membered rings:

  • Space group: R-3c (No. 167)
  • Crystal system: trigonal
  • Lattice parameters:
    • a = b = 8.72922 Å, c = 17.06581 Å
    • α = β = 90°, γ =120°

 Here, you can download the CIF.

Literature:

[1] H. Engelhardt and B. Kamb, Structure of ice IV, a metastable high-pressure phase, Journal of Chemical Physics 1981, 75, 5887-5899. DOI: 10.1063/1.442040

[2] C. G. Salzmann, I. Kohl, T. Loerting, E. Mayer and A. Hallbrucker, Raman spectroscopic study on hydrogen-bonding in recovered ice IV, Journal of Physical Chemistry B 2003, 107, 2802-2807. DOI: 10.1021/jp021534k

 

[Atomistic 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).

and

CrystalMaker®.]

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Ice III and IX

Ice III and IX (Ice three and Ice nine)

  • Ice III can be formed from liquid water at 300 MPa (3000 bar) by lowering the temperature to approx. 250 K.
  • The relative permittivity is very high (~ 117)
  • Density: 1.16 g/cm3

Structural features

  • Ice III is also called Keatite Ice, because the oxygen atoms are located at analogous positions of the silicon atoms in the SiO2 phase Keatite.
  • Ice IX is the proton-ordered form of Ice III.
  • The tetrahedral environment of the water molecules are considerably distorted.
  • Interestingly, there are no 6-membered rings present anymore, but 5, 7, and 8 –membered rings instead. The 5-membered rings can be best seen if you look along the a or b direction:

 

    • Two-third of the water molecules are forming 41 helices/screws running along the c axis, which means that Ice III is chiral! The other water molecules connect these helices and are forming a 21 helix.

 

  • Space group: P41212 (No. 92)
  • Crystal system: tetragonal
  • Lattice parameters:
    • a = b = 6.73(1) Å, c = 6.83(1) 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).

and

CrystalMaker®.

Ice II (Ice-two)

Ice II (Ice two)

  • can be formed from hexagonal Ice (Ice Ih) at 198 K and 3000 bar or by decompressing Ice-five (Ice V) at 238 K
  • Ice II is likely to be a major rock-forming mineral in the outer Solar System
  • It may form a major proportion of icy moons such as Jupiter’s Ganymede
  • Density: 1.16 g/cm3

Structural features:

  • Ice-two is a proton-ordered form of ice
  • there are two types of 6-membered rings; one is almost flat (Type A) the other one has a more puckered, chair-like conformation (Type B)
  • these two types of rings are strictly alternating stacked along the c axis

  • If you look along the c axis, you will see that the two types of 6-rings are slightly rotated against each other (~ 16 degrees)

  • Space group R-3
  • Lattice parameters:
    • a = b = 12.935 Å, c = 6.233 Å
    • α = β = 90°γ = 120°

  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).]

Ice Ic

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).]

Ice Ih

Ice Ih (Ice one hexagonal)

Structural features:

  • single molecule and molecular arrangement

  • Ice Ih is a proton-disordered phase

  • every water molecule is involved in 4 H-bonds (2 acceptors, 2 donors)
  • tetrahedrally coordinated
  • O-H bond length approx. 99 pm
  • H …. O-H distance approx. 175 pm
  • O … O distance approx. 275 pm
  • H-bond strength: approx. 21 kJ/mol
  • 6-membered rings
    • chair-like conformation in the (a,b) plane
    • boat-like conformation along the c direction

(graphic 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).

  • sometimes called “tridymite ice” because the oxygen atoms occupy the Si analogeous positions in the SiO2 phase tridymite
  • Space group P63/mmc
    • a = b = 4.4975 Å, c = 7.3224 Å
    • α = β = 90°, γ = 120°

 Here, you can download the CIF.