Title of article
Deformation of polycrystalline iron up to 30 GPa and 1000 K
Author/Authors
Merkel، نويسنده , , Sébastien and Wenk، نويسنده , , Hans-Rudolf and Gillet، نويسنده , , Philippe and Mao، نويسنده , , Ho-kwang and Hemley، نويسنده , , Russell J.، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2004
Pages
13
From page
239
To page
251
Abstract
Angle-dispersive radial X-ray diffraction measurements were conducted on α- and ϵ-Fe under nonhydrostatic stress conditions up to 30 GPa and 1000 K in laser heated diamond anvil cells. α-Fe (bcc) is found to develop preferred orientation compatible with observations under ambient conditions. The preferred orientation of the α-phase is inherited by the ϵ-phase (hcp) in accordance with the Burgers orientation relationship. A comparison between the observed texture in ϵ-Fe with results from polycrystal plasticity modeling suggests that the predominant deformation mechanisms are basal slip (0 0 0 1)〈1̄ 2 1̄ 0〉 and prismatic slip {1 0 1̄ 0}〈1̄ 2 1̄ 0〉, presumably associated with minor mechanical twinning. We do not observe any evidence of slip on the {1 1 2̄ 2}〈1 1 2̄ 3〉 system that was proposed based on analogies with Cr–Ni stainless steel. Finally, we do not observe any change in preferred orientation upon heating in situ at 28 GPa and 1000 K.
Keywords
Anisotropy , Earth core , high pressure , Iron , Deformation , Slip system , Texture
Journal title
PHYSICS OF THE EARTH AND PLANETARY INTERIORS
Serial Year
2004
Journal title
PHYSICS OF THE EARTH AND PLANETARY INTERIORS
Record number
2303816
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