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
Link To Document :
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