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@ARTICLE{Mazur:288328,
author = {Mazur, K. and Wieteska, K. and Wierzchowski, W. and
Sarnecki, J. and Lipiński, D. and Brzozowski, A. and
Paulmann, C.},
title = {{H}igh {R}esolution {X}-{R}ay {D}iffractometric,
{T}opographic and {R}eflectometric {S}tudies of {E}pitaxial
{L}ayers on {P}orous {S}ilicon {D}estined for {E}xfoliation},
journal = {X-ray spectrometry},
volume = {44},
number = {5},
issn = {0049-8246},
address = {New York, NY [u.a.]},
publisher = {Wiley},
reportid = {PUBDB-2015-04924},
pages = {363-370},
year = {2015},
note = {(c) John Wiley $\&$ Sons, Ltd.},
abstract = {The presently studied substrates for manufacturing
freestanding silicon epitaxial layers contained two porous
layers with different porosities. The upper layers of
significantly lower porosity after annealing provided smooth
surfaces for deposition of epitaxial layers and the deeper
layers of greater porosity enabling easier exfoliation
epitaxial foil. The layered structures have been studied by
means of synchrotron diffraction topography and by recording
of rocking curves from small local area. The most effective
method of revealing defects in freestanding exfoliated
layers were Bragg-case projection topographs and ‘zebra’
pattern monochromatic beam topographs providing a map of
sample curvature. The samples have been additionally
examined by means of high-resolution diffractometry and
reflectometry.The porous layers without epitaxial deposition
provided strong narrow maximum at low angle side of the
substrate maximum common for both of the porous layers. The
most probable effect of the deposition of epitaxial layer is
the decrease of lattice parameter in the upper layer with
lower porosity, which provided the maxima in the diffraction
curves located on low angle side of the substrate maximum.
The topographic investigations revealed some defects in
deposited epitaxial layers, connected with some
irregularities of the annealed porous layer. Very
characteristic common defects were large caverns, overgrown
in the epitaxial process with the diameters of several
tenths of micrometers and defects (possibly the overgrown
submicron caverns), associated with some bundles of
dislocations resolved in the topographs. In layers of large
thickness, the characteristic long black and white stripes
along <110> have also been observed, which most probably
were stacking faults with dislocation loops.},
cin = {DOOR},
ddc = {530},
cid = {I:(DE-H253)HAS-User-20120731},
pnm = {899 - ohne Topic (POF3-899)},
pid = {G:(DE-HGF)POF3-899},
experiment = {EXP:(DE-H253)D-E2-20150101 / EXP:(DE-H253)D-F1-20150101},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000360088600009},
doi = {10.1002/xrs.2641},
url = {https://bib-pubdb1.desy.de/record/288328},
}