Abstract
Ice single crystals were deformed under torsion and dislocation arrangements were analyzed by synchrotron topography at ESRF (European Synchrotron Radiation Facility). Profile analysis of the topographs revealed the scale-invariant character of the dislocation arrangement with long-range correlations. Dislocation density gradients are shown to be slightly anti-correlated as the intensity profile is similar to an anti-persistent random walk-like signal. This analysis reveals the influence of internal stresses on dislocation arrangement up to the sample scale. Similar observations in reversed torsion experiments, together with strong hardening behaviour, allow a mechanism of cross-slip of basal dislocations on prismatic planes to be suggested for interpretation of local dislocation interaction behaviour.
Acknowledgements
We are very thankful to the ESRF organization and more particularly to Jürgen Härtwig and José Baruchel from ID19 beamline. We would also like to thank Juliette Chevy and Marc Fivel for fruitful discussions. Also, many thanks to the two referees for valuable comments which helped improving the quality of the paper.