TY - JOUR
T1 - Specular reflection intensity modulated by grazing-incidence diffraction in a wide angular range
AU - Nikolaev, K. V.
AU - Makhotkin, I. A.
AU - Yakunin, S. N.
AU - Van De Kruijs, R. W.E.
AU - Chuev, M. A.
AU - Bijkerk, F.
N1 - Wiley deal
PY - 2018/9/1
Y1 - 2018/9/1
N2 - Grazing-incidence X-ray diffraction (GID) is a well known technique for the characterization of crystal surfaces. A theoretical study has been performed of the sensitivity of GID to the structure of a crystal surface and distorted nanometre-thin surface layers. To simulate GID from crystals that have a complex subsurface structure, a matrix formalism of the dynamical diffraction theory has been applied. It has been found that the azimuthal rocking curves of a crystal that has a distorted subsurface, measured over a wide angular range, show asymmetric thickness oscillations with two distinguishable sets of frequencies: one corresponding to the diffraction in the single-crystal subsurface layer and the second corresponding to the diffraction in the single-crystal substrate. Therefore, azimuthal rocking curves allow characterization of the subsurface structure of a single crystal. Furthermore, thickness oscillations induced by evanescent diffraction modulate the specular reflection intensity, showing high-intensity modulations. This will potentially allow implementation of subsurface crystal characterization using, for instance, a laboratory-scale X-ray diffractometer.
AB - Grazing-incidence X-ray diffraction (GID) is a well known technique for the characterization of crystal surfaces. A theoretical study has been performed of the sensitivity of GID to the structure of a crystal surface and distorted nanometre-thin surface layers. To simulate GID from crystals that have a complex subsurface structure, a matrix formalism of the dynamical diffraction theory has been applied. It has been found that the azimuthal rocking curves of a crystal that has a distorted subsurface, measured over a wide angular range, show asymmetric thickness oscillations with two distinguishable sets of frequencies: one corresponding to the diffraction in the single-crystal subsurface layer and the second corresponding to the diffraction in the single-crystal substrate. Therefore, azimuthal rocking curves allow characterization of the subsurface structure of a single crystal. Furthermore, thickness oscillations induced by evanescent diffraction modulate the specular reflection intensity, showing high-intensity modulations. This will potentially allow implementation of subsurface crystal characterization using, for instance, a laboratory-scale X-ray diffractometer.
KW - UT-Hybrid-D
KW - Crystal surface
KW - GID
KW - Grazing-incidence X-ray diffraction
KW - Specular reflection
KW - Azimuthal rocking curves
UR - http://www.scopus.com/inward/record.url?scp=85052959351&partnerID=8YFLogxK
U2 - 10.1107/S2053273318008963
DO - 10.1107/S2053273318008963
M3 - Article
AN - SCOPUS:85052959351
SN - 0108-7673
VL - 74
SP - 545
EP - 552
JO - Acta Crystallographica Section A: Foundations and Advances
JF - Acta Crystallographica Section A: Foundations and Advances
IS - 5
ER -