Residual strain orientation in rolled titanium determined with synchrotron X-ray Laue microdiffraction

被引:0
|
作者
Devoe, Michelle [1 ]
Tamura, Nobumichi [2 ]
Wenk, Hans-Rudolf [1 ]
机构
[1] Univ Calif Berkeley, Earth & Planetary Sci, Berkeley, CA 94720 USA
[2] Lawrence Berkeley Natl Lab, Adv Light Source, Berkeley, CA 94720 USA
来源
基金
美国国家科学基金会;
关键词
stress; strain; residual stress; residual strain; X-ray synchrotron radiation; Laue diffraction; MICROBEAM MEASUREMENTS; PLASTIC-DEFORMATION; DEFORMED-CRYSTALS; LATTICE STRAIN; STRESS; DIFFRACTION; DISLOCATIONS; EVOLUTION; PROGRAM; ALLOYS;
D O I
10.1107/S1600576722011311
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Previously, synchrotron X-ray Laue microdiffraction has been used to measure the magnitudes of residual strain in materials. Recently the method was advanced to determine the orientation of the strain ellipsoid and applied to naturally deformed quartzites; however, the deformation history of these quartzites is ambiguous due to their natural origin. In this study, synchrotron X-ray Laue microdiffraction (mu XRD) is used to measure the residual strain for the first time in a sample with known stress history, rolled titanium. A deviatoric strain tensor is calculated from each Laue diffraction image collected with two mXRD scans of a rolled titanium sheet in different sample orientations. The principal strain axes are calculated using an eigen decomposition of the deviatoric strain tensors. The results show that the principal axis of compression is aligned with the normal direction of the titanium sheet, and the principal axis of extension is aligned with the rolling direction. Pole figures are used to represent the 3D distribution of residual strain axes.
引用
收藏
页码:135 / 142
页数:8
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