1980
DOI: 10.1107/s0021889880012472
|View full text |Cite
|
Sign up to set email alerts
|

Crystal subgrain misorientations observed by X-ray topography in reflection

Abstract: Based on the principles of conservation of momentum and energy for X-ray diffraction, a vector description is obtained for the displacement of adjacent subgrain images in reflection topographs. The analysis includes, in addition to those crystal parameters defining the misorientation at a subgrain boundary, the combined effects of (horizontal and vertical) divergence in the incident X-ray beam and of the position where the Xray images are recorded. The vector description is matched with a stereographic project… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

1981
1981
2023
2023

Publication Types

Select...
8

Relationship

1
7

Authors

Journals

citations
Cited by 42 publications
(3 citation statements)
references
References 8 publications
0
3
0
Order By: Relevance
“…A similar analysis to that described for zinc was reported for the preferred [010] orientation of crystal subgrain boundary misorientations in the solidification of nickel single crystals [25]. Figure 8 shows the diffraction geometry developed in a wave vector description of two subgrain reflections being obtained with an asymmetric crystal topography (ACT) system.…”
Section: X-ray Topography Of Symmetrical-tilt Crystal Subgrain Boundamentioning
confidence: 56%
“…A similar analysis to that described for zinc was reported for the preferred [010] orientation of crystal subgrain boundary misorientations in the solidification of nickel single crystals [25]. Figure 8 shows the diffraction geometry developed in a wave vector description of two subgrain reflections being obtained with an asymmetric crystal topography (ACT) system.…”
Section: X-ray Topography Of Symmetrical-tilt Crystal Subgrain Boundamentioning
confidence: 56%
“…This is different from the case of the PO and PT twins, where a set oftopographs have zero displacement of domain images. Here, we do not intend to demonstrate the topographic characteristic of 120 ° domains, but we only take such domain structure as a example to provide a general way for calculation of the magnitude and direction of the image displacement related to any two misoriented domains [or even crystal subgrains (Armstrong, Boettinger & Kuriyama, 1980)], based on the Cartesian representations of the two misoriented reciprocal lattices and the direction of the incident beam. As the displacement vectors are determined, the orientation contrast in any reflections can be explained easily.…”
Section: ° Domains In Perovskite Crystalmentioning
confidence: 99%
“…However, even where the difference in orientation is in excess of several arc-minutes, simultaneous diffraction from more than one grain can be observed and analyzed quantitatively if the crystal is suitably oriented with respect to the beam, as has been done in figure 9 , where five grains can be distinguished. In such instances, the tilt of the individual grains and their orientation with respect to one another can be accurately determined from the clear displacement of the images of the various grains with respect to each other [ 16 ].…”
Section: Illustrative Examplesmentioning
confidence: 99%