Skip to main content
  • ENG
  • Chinese
  • Home
  • News
  • Material blog
  • Research
    • Science
    • Neutron scattering
    • Computer simulations
    • Theoretical studies
  • Documents
    • Career
    • Research presentations
    • Teaching materials
  • Personal
    • Career
  • Pictures
  • Contact me

Cristobalite, cubic-SiO2

June 15, 2019 at 5:31 pm, No comments
Silica, SiO2, is one of the most common materials on the Earth's crust. The most common form is quartz, which is the material that keeps the time in everyone's watch and clock. At high temperature quartz transforms to the phase known as cristobalite. In its crystal structure the silicon atoms occupy  the same places in the diamond structure (like crystalline silicon), with the oxygen atoms half-way  between neighbouring silicon atoms. As a result, each silicon atom is surrounded by four oxygen atoms to make SiO4 tetrahedra, and all tetrahedra are connected together in one near-infinite network sharing corners.

  
The figures above show the arrangement of atoms (left; blue are silicon and red are oxygen) and SiO4 tetrahedra (right).

It can be seen from the picture that the bonds between oxygen atoms and two neighbouring silicon atoms line in straight lines. This arrangement is not common in similar silicate materials, and calculations show that it is energetically unfavourable. These materials prefer a bond angle of around 145° rather than 180°. To achieve this the oxygen atoms must be displaced in there perpendicular direction, giving rise to disorder in the crystal structure. At low temperature the cubic structure transforms into a lower-symmetry tetragonal structure which has the normal Si–O–Si bond angles. But at high temperature, the disorder is dynamic.

We have looked at the phase transition in cristobalite and the structure of its high-temperature phase using a variety of methods. Using molecular dynamics simulations and neutron total scattering methods coupled with the Reverse Monte Carlo method we have 

Methods

Crystal structures were analysed by neutron powder diffraction. Cristobalite was the first material I studied using the neutron total scattering method and to which we applied the Reverse Monte Carlo method. 

Collaborators

My first collaborator in the study of cristobalite was Ian Swainson, one of my first PhD students in Cambridge. Neutron total scattering and RMC work was carried out in collaboration with Matt Tucker (now Oak Ridge National Laboratory, USA) and David Keen (ISIS neutron tactility, UK).

References

Landau free energy and order parameter behaviour of the α/β phase transition in cristobalite. WW Schmahl, IP Swainson, MT Dove and A Graeme-Barber. Zeitschrift für Kristallographie 201, 125–145, 1992 (https://doi.org/10.1524/zkri.1992.201.1-2.125)

Low-frequency floppy modes in β-cristobalite. IP Swainson and MT Dove. Physical Review Letters 71, 193–196, 1993 (https://doi.org/10.1103/PhysRevLett.71.193)

Molecular dynamics simulation of α- and β-cristobalite. IP Swainson and MT Dove. Journal of Physics: Condensed Matter 7, 1771–1788, 1995 (https://doi.org/10.1088/0953-8984/7/9/005)

Direct measurement of the Si–O bond length and orientational disorder in β cristobalite. MT Dove, DA Keen, AC Hannon and IP Swainson. Physics and Chemistry of Minerals 24, 311–317, 1997 (https://doi.org/10.1007/s002690050043)

Rigid Unit Modes and dynamic disorder: SiO2 cristobalite and quartz. M Gambhir, MT Dove and V Heine. Physics and Chemistry of Minerals 26, 484–495, 1999 (https://doi.org/10.1007/s002690050211)

Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2. MT Dove, MS Craig, DA Keen, WG Marshall, SAT Redfern, KO Trachenko, MG Tucker. Mineralogical Magazine 64, 569–576, 2000 (https://doi.org/10.1180/002646100549436)

Dynamic structural disorder in cristobalite: Neutron total scattering measurement and Reverse Monte Carlo modelling. MG Tucker, MD Squires, MT Dove and DA Keen. Journal of Physics: Condensed Matter 13, 403–423, 2001 (https://doi.org/10.1088/0953-8984/13/3/304)

Infrared and Raman spectroscopy studies of the α–β phase transition in cristobalite. IP Swainson, MT Dove, and DC Palmer. Physics and Chemistry of Minerals, 30, 353–365, 2003 (https://doi.org/10.1007/s00269-003-0320-8)

Evaluation of domain models for β-cristobalite from the pair distribution function. ER Cope and MD Dove. Journal of Physics: Condensed Matter 22, 125401, 2010 (https://doi.org/10.1088/0953-8984/22/12/125401)

No comments

Leave a reply







Recent Posts

  • Thermal disorder and bond anharmonicity in cesium lead iodide studied by neutron total scattering and the Reverse Monte Carlo method
    28 Jun, 2019
  • Cristobalite, cubic-SiO2
    15 Jun, 2019
  • Malononitrile, CH2(CN)2
    15 Jun, 2019
Created with Mozello - the world's easiest to use website builder.

Create your website or online store with Mozello

Quickly, easily, without programming.

Report abuse Learn more