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Multiscale 3D characterization with dark-field x-ray microscopy

Published online by Cambridge University Press:  08 June 2016

Hugh Simons
Affiliation:
Department of Physics, Technical University of Denmark, Denmark; husimo@fysik.dtu.dk
Anders Clemen Jakobsen
Affiliation:
Department of Physics, Technical University of Denmark, Denmark; andcj@fysik.dtu.dk
Sonja Rosenlund Ahl
Affiliation:
Department of Physics, Technical University of Denmark, Denmark; sroh@fysik.dtu.dk
Carsten Detlefs
Affiliation:
European Synchrotron Radiation Facility, France; detlefs@esrf.fr
Henning Friis Poulsen
Affiliation:
Department of Physics, Technical University of Denmark, Denmark; hfpo@fysik.dtu.dk

Abstract

Dark-field x-ray microscopy is a new way to three-dimensionally map lattice strain and orientation in crystalline matter. It is analogous to dark-field electron microscopy in that an objective lens magnifies diffracting features of the sample; however, the use of high-energy synchrotron x-rays means that these features can be large, deeply embedded, and fully mapped in seconds to minutes. Simple reconfiguration of the x-ray objective lens allows intuitive zooming between different scales down to a spatial and angular resolution of 100 nm and 0.001°, respectively. Three applications of the technique are presented—mapping the evolution of subgrains during the processing of plastically deformed aluminum, mapping domains and strain fields in ferroelectric crystals, and the three-dimensional mapping of strain fields around individual dislocations. This ability to directly characterize complex, multiscale phenomena in situ is a key step toward formulating and validating multiscale models that account for the entire heterogeneity of materials.

Information

Type
Research Article
Copyright
Copyright © Materials Research Society 2016 
Figure 0

Figure 1. Principle of dark-field x-ray microscopy. Monochromatic x-rays illuminate a crystalline element of interest, and the diffracted radiation is imaged by means of an x-ray objective and a 2D detector. The magnification is approximately given by the ratio q′/p′. Scanning the sample tilt (α, β) and 2θ angles facilitates mapping of orientation and strain, respectively, while different projection angles can be obtained by rotating the sample around its scattering vector, Q.22

Figure 1

Figure 2. Multiscale mapping of 10% tensile deformed 1050 (99.5% pure) aluminum. (a) Part of a map of all grains in the specimen. (b) Zooming in on one grain and mapping the intrinsic variation in orientation. A vertical section through the grain is shown. (c) Additional zoom and mapping of selected individual subgrains in 3D. The spatial resolution from left to right is 3.5 µm, 1.5 µm, and 300 nm, and the angular resolution is 0.5°, 0.15°, and 0.03°, respectively. The colors symbolize orientations.22

Figure 2

Figure 3. Structure of one layer of a recrystallized grain within a ∼500-µm-sized 1050 (99.5% pure) aluminum sample. The distribution of angular spread of the (200) reflection is recorded for each voxel in terms of sample tilt (α, β) (as per Figure 1). (a) Map of the most intense angular setting for each voxel, (b) corresponding map of local misorientations, and (c) map of the full width at half maximum (FWHM) of the mosaic distribution for each voxel.23

Figure 3

Figure 4. Histograms of subgrain size (defined as the equivalent spherical radius, Req) as a function of a linear increase in temperature during recovery of 1050 (99.5% pure) aluminum. The distribution is prone to experimental error below a radius of 1 µm.24

Figure 4

Figure 5. Reciprocal space map around the 220 reflection of a KNbO3 ferroelectric crystal obtained as a rapid prescanning technique. The peaks correspond to the lattice spacing and orientation of domain variants. Qx and Qy are the reciprocal space directions corresponding to α and β. The contours correspond to a normalized log axis, where red is the highest intensity value.28

Figure 5

Figure 6. False-color maps of (a) orientation and (b) strain in the KNbO3 crystal. Zoomed in images of the (c) orientation and (d) strain from the centers of the maps show local gradients around stripe-like domains. The orientation and strain maps correspond to the same region of the sample and are shown at the same scale. The local orientation in terms of sample tilt (α, β) (as per Figure 1) in (a) and (c) corresponds to the keys in the bottom left corner of the images. The local lattice strain in (b) and (d) corresponds to the key on the right side of the images.28

Figure 6

Figure 7. False-color image of three dislocations within a diamond crystal. Two images are superposed, the red and blue ones representing an offset in the axial strain of +3 × 10–4 and –3 × 10–4, respectively. The sample was fully illuminated and, as such, the image is a projection.34