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Related Experiment Videos

Imaging dislocations in ice.

I Baker1

  • 1Thayer School of Engineering, Dartmouth College, Hanover, New Hampshire 03755, USA.

Microscopy Research and Technique
|August 26, 2003
PubMed
Summary
This summary is machine-generated.

Synchrotron X-ray topography reveals ice crystal deformation mechanisms. Dynamic studies show basal slip by screw and edge dislocations, with generation at grain boundaries in polycrystals.

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Area of Science:

  • Materials Science
  • Solid State Physics
  • Crystallography

Background:

  • Dislocations govern ice crystal mechanical properties.
  • Previous studies used etch pitting, TEM, and conventional X-ray topography (XT).
  • Conventional XT images dislocations that have already recovered.

Purpose of the Study:

  • To investigate dislocation dynamics in ice using advanced X-ray topography.
  • To elucidate deformation mechanisms in single crystal and polycrystalline ice.
  • To measure dislocation velocities and characterize dislocation generation.

Main Methods:

  • High-intensity synchrotron X-ray topography (SXRT) for dynamic in situ observations.
  • Comparison with conventional X-ray topography, transmission electron microscopy, and etch pitting-replication.

Related Experiment Videos

  • Deformation experiments on ice single crystals and polycrystals.
  • Main Results:

    • SXRT revealed slip primarily occurs on the basal plane via screw and 60° (1/3)[1120] dislocations in single crystals.
    • Non-basal slip by edge dislocations was also observed.
    • Dislocation multiplication sources (e.g., Frank-Read) were demonstrated, and velocities measured.
    • In polycrystals, dislocation generation initiated at grain boundaries.
    • Faulted dislocation loops were predominantly interstitial in both crystal types.

    Conclusions:

    • Synchrotron X-ray topography is the premier technique for studying dynamic dislocation behavior in ice.
    • Understanding dislocation mechanisms is crucial for predicting ice's mechanical response.
    • Grain boundaries act as critical sites for dislocation generation in polycrystalline ice.