Publication details

X-ray rocking curve imaging on large arrays of extremely tall SiGe microcrystals epitaxial on Si

Authors

MEDUŇA Mojmír CAHA Ondřej CHOUMAS Emanuil BRESSAN Franco VON KÄNEL Hans

Year of publication 2021
Type Article in Periodical
Magazine / Source Journal of Applied Crystallography
MU Faculty or unit

Faculty of Science

Citation
Web https://doi.org/10.1107/S1600576721004969
Doi http://dx.doi.org/10.1107/S1600576721004969
Keywords rocking curve imaging; patterned Si substrates; Ge microcrystals; X-ray diffraction; thermal strain relaxation
Description This work investigates layers of densely spaced SiGe microcrystals epitaxially formed on patterned Si and grown up to extreme heights of 40 and 100 mm using the rocking curve imaging technique with standard laboratory equipment and a 2D X-ray pixel detector. As the crystalline tilt varied both within the epitaxial SiGe layers and inside the individual microcrystals, it was possible to obtain real-space 2D maps of the local lattice bending and distortion across the complete SiGe surface. These X-ray maps, showing the variation of crystalline quality along the sample surface, were compared with optical and scanning electron microscopy images. Knowing the distribution of the X-ray diffraction peak intensity, peak position and peak width immediately yields the crystal lattice bending locally present in the samples as a result of the thermal processes arising during the growth. The results found here by a macroscopic-scale imaging technique reveal that the array of large microcrystals, which tend to fuse at a certain height, forms domains limited by cracks during cooling after the growth. The domains are characterized by uniform lattice bending and their boundaries are observed as higher distortion of the crystal structure. The effect of concave thermal lattice bending inside the microcrystal array is in excellent agreement with the results previously presented on a microscopic scale using scanning nanodiffraction.
Related projects:

You are running an old browser version. We recommend updating your browser to its latest version.

More info