G. Bhagavannarayana et P. Zaumseil, DIFFUSE-X-RAY SCATTERING OF MISFIT DISLOCATIONS AT SI1-XGEX SI INTERFACES BY TRIPLE-CRYSTAL DIFFRACTOMETRY/, Journal of applied physics, 82(3), 1997, pp. 1172-1177
Heterostructure Si1-xGex layers on (001)Si substrates with different d
egrees of relaxation R, ranging from the nearly pseudomorphic state to
the nearly relaxed state (R similar to 0.8), were characterized by di
ffuse x-ray scattering measurements. The lattice constants a(perpendic
ular to) and a(parallel to), and from these the Ge content x, the rela
xation A, and misfit dislocation density D-d, were determined by singl
e crystal diffractometry. The thickness of the SiGe layers was measure
d in the as-grown state by double crystal diffractometry. A standard t
riple crystal x-ray diffractometer was used to analyze the diffuse x-r
ay scattering (DXS) intensity by rotation of the analyzer crystal (Del
ta Theta) at a fixed sample position (alpha). The intensities were mea
sured around the 004 reciprocal lattice point of the Si substrate usin
g a wide open counter and a wide range of rotation angle (Delta Theta)
for the analyzer crystal, The diffuse scattering increases steeply wi
th increasing dislocation density up to a critical value of D-d approx
imate to 5 x 10(4) cm(-1). Then it reaches saturation and decreases sl
owly as D-d increases. This behavior can be cm explained by the superp
osition of the strain fields of neighboring dislocations above a criti
cal density, so that only the heavily distorted regions near the dislo
cation core participate in scattering. This is confirmed by the fact t
h-dt the DXS measured for different alpha values follows The Stokes-Wi
lson scattering (I(DXS)proportional to q(-4); q being the scattering v
ector). We show that: the diffuse scattering technique is a very sensi
tive tool to detect relaxation at relatively low levels of dislocation
densities , where diffractometric techniques that measure the lattice
constants are D-d less than 5x10(4) cm(-1), near their resolution lim
its. (C) 1997 American Institute of Physics.