H.-R. Wenk
W.B. Durham
L.A. Stern
S. H. Kirby
K. Bennett
1997
<p>The preferred crystallographic orientation developed during the ice I ← II transformation and during the plastic flow of ice II was measured in polycrystalline deuterium oxide (D<sub>2</sub>O) specimens using low-temperature neutron diffraction. Samples partially transformed from ice I to II under a non-hydrostatic stress developed a preferred crystallographic orientation in the ice II. Samples of pure ice II transformed from ice I under a hydrostatic stress and then when compressed axially, developed a strong preferred orientation of compression axes parallel to (10<span class="overline">1</span>0). A match to the observed preferred orientation using the viscoplastic self-consistent theory was obtained only when (10<span class="overline">1</span>0) [0001] was taken as the predominant slip system in ice II.</p>
application/pdf
10.1080/01418619708209983
en
Taylor & Francis
Preferred crystallographic orientation in the ice I ← II transformation and the flow of ice II
article