Minerals Science Course B Reciprocal Space, Symmetry and Crystallography
Properties of X-rays - Stanford University · PDF file2Theta/Omega (°) Fringe Period...
Transcript of Properties of X-rays - Stanford University · PDF file2Theta/Omega (°) Fringe Period...
High-Resolution XRD
What is thin film/layer?
Material so thin that its characteristics are dominated primarily by two dimensional effects and are mostly different than its bulk propertiesSource: semiconductorglossary.com
Material which dimension in the out-of-plane direction is much smaller than in the in-plane direction.
A thin layer of something on a surfaceSource: encarta.msn.com
Epitaxial Layer
A single crystal layer that has been deposited or grown on a crystalline substrate having the same structural arrangement.Source: photonics.com
A crystalline layer of a particular orientation on top of another crystal, where the orientation is determined by the underlying crystal.
Homoepitaxial layerthe layer and substrate are the same material and possess the same lattice parameters.
Heteroepitaxial layerthe layer material is different than the substrate and usually has different lattice parameters.
Accessible Information to X-ray Diffraction
Definition for structural types
Structure Type Definition
Perfect epitaxial Single crystal in perfect registry with the substrate that is also perfect.
Nearly perfect epitaxialSingle crystal in nearly perfect registry with the substrate that is also nearly perfect.
Textured epitaxialLayer orientation is close to registry with the substrate in both in-plane and out-of-plane directions. Layer consists of mosaic blocks.
Textured polycrystallineCrystalline grains are preferentially oriented out-of-plane but random in-plane. Grain size distribution.
Perfect polycrystalline Randomly oriented crystallites similar in size and shape.
Amorphous Strong interatomic bonds but no long range order.
P.F. Fewster X-ray Scattering from Semiconductors
Accessible Information to X-ray Diffraction
Defects that are common in epilayer structures
Crystalline state of the layers:
Epitaxial (coherent with the substrate, relaxed)
Polycrystalline (random orientation, preferred orientation)
Amorphous
Crystalline quality
Strain state (fully or partially strained, fully relaxed)
Defect structure
Chemical composition
Thickness
Surface and/or interface roughness
What we want to know about thin films?
Accessible Information to X-ray Diffraction
Structural parameters that characterize various material types
parameters that have meaning parameters that could have meaning
Thickness Composition Relaxation DistortionCrystalline
sizeOrientation Defects
Perfect epitaxy
Nearly perfect epitaxy
Textured epitaxy
Textured polycrystalline
Perfect polycrystalline
Amorphous
Accessible Information to X-ray Diffraction
Mismatch
Consider two materials with the same space group, same atomic arrangements, but slightly different lattice parameters and elastic parameters.
aL
aL=aS
aS
aS
aS
aS
cL
aL
Beforedeposition
Afterdeposition
Mismatch
The peak separation between substrate and layer is related to the change of interplanarspacing normal to the substrate.
If it is 00L reflection then the experimental x-ray mismatch:
S
SL
d
dd
d
d
a
am*
True lattice mismatch is:
s
s
R
L
a
aam
Relationship:
1
1*mm
Poisson ratio 2
*
3
1
mm
a llL=aS
aS
aS
a L
Relaxation
The problems occur when the elastic parameters are incapable of accommodating the distortions necessary for perfect epitaxy.
aS
aS
cL cL
aS
aS
Fully or partially relaxed Fully or partially relaxed and tilted
Beforedeposition
AfterdepositionR
L
R
LL
R
L
R
LLzz
d
dd
a
aa
Tetragonal Distortion
Lattice mismatch betweencubic lattice parameters:
S
S
R
L
a
aa
a
a
Lattice mismatch induces lattice strain:
R
La
R
La
SaSa
Lc
SL aa
SaSa
R
LaR
La
SaSa
0
0
Relaxed
Strained, coherent, pseudomorphic
Partially relaxed
(000)
(00l)
(100)
(10l)
(200)
(20l)
Cubic: aL> aS
Cubic
Relaxed Layer
(000)
(00l)
(100)
(10l)
(200)
(20l)
Tetragonal: aIIL = aS, a
L > aS
Cubic
Strained Layer
Tetragonaldistortion
Cubic
Cubic
Cubic
Tetragonal
ReciprocalSpace
(000) (000)
(00l) (00l)
(hkl) (hkl)
aL > aS
Perfect Layers: Relaxed and Strained
Strain
Si(004)
SiGe(004)
F. C. Frank and J. H. van der Merwe, Proc. R. Soc. London, Ser. A 198, 216 (1949).
avezz
yyxxzz
y
L
y
L
y
L
yy
x
L
x
L
x
L
xx
z
L
z
L
z
L
zz
R
R
R
R
R
R
d
dd
d
dd
d
dd
1
2
1
Composition
Vegard's law
Vegards law states that the lattice parameter of substitutional solid solution varies linearly between the lattice parameter values for the components. The composition is expressed in atomic percentage.
R
B
R
A
R
BA axxaa xx )1(1
Composition
R
B
R
A
R
B
R
BA
R
B
R
A
R
BA
aa
aax
axxaa
xx
xx
1
1)1(
For Si1xGex: 1 = + 1 + 0.007 2 12 1
Si(004)
SiGe(004)
S
SS
z
S
z
S
z
L
S
S
S
S
R
L
d
dd
a
aam
ma
aam
sin
sinsin*
1
1*
Si(004)
SiGe(004)
2 =
=
2
= +
=
For out-of-plane lattice parameter:
Braggs law:
can be calculated from Braggs law knowing = 5.431
Layer Tilt
If the layer is tilted relative to the substrate then this will result in a shift of the layer peak relative to that of the substrate.
This is not connected with the composition.
2
1800
Then true splitting mismatch:
mismatch peak splitting a tilt angle rotation angle
The resulting layer peak splitting will depend on:
If specimen is rotated by angle about its normal the layer peak will be displaced by:
180180
00
cos
cos
a
a
Layer Relaxation
Our layer is completely coherent.
In this case it is enough to measure misfit only along (00l ) direction.
Partially or fully relaxed layers.
We need to measure misfit parallel to the interface as well as perpendicular.
For this we need an asymmetric reflection (e.g. 224, 113).
Layer Relaxation
The effect of tilt on the peak splitting is reversed if the specimen is rotated by 180o about its surface normal.
The splitting due to mismatch will not be affected by such rotation.
We can make grazing incidence or grazing exit measurements to separate the tilt from the true splitting.
Relaxation
The resulting measured splittings are now different between these two geometries:
gi grazing incidence
grazing exit ge
We need to know the lattice parameter of the layer parallel and perpendicular to the substrate: aL , bL , and cL . From these we may calculate the relaxation and the fully relaxed lattice parameter aS .
Consider aL = bL (tetragonal distortion).
SL
SL
angle between reflecting plane and the surface
Relaxation
sin2
12
2
2
22
2
d
c
l
a
kh
d LLhkl
Using interplanar spacing equation and Bragg law:
we obtain cell constants for the layer (001 oriented):
2
22
sinsin2
cossin2
l
khla
lc
LL
L
LL
L
Relaxation
The relaxation is defined as:
100
xx
xx
S
R
L
SL
aa
aaR
R
Lxa the fully relaxed in-plane lattice parameter of the epilayer.
1
21
R
L
L
R
LR
LL
x
xx
xz a
aaaa
R
Lxa is the value that is used in Vegards law to find the composition of the epilayer.
yyxxzz
1
121
12
xz
x
LLR
L
aa
a
For cubic lattice:R
L
L
R
L
yyxxa
aax
R
L
L
R
L
zza
aaz
and
Then:
Substrate misorientation
Substrates are often specified at some angle from (001) or (111).
This may need to be verified.
2
21
Rotation of the surface plane through 180o between measurements
If we do measurements at 0o and 180o to get 0 and at 90o and 270o to get 90, then
maximum max is given by:
0
90max
90
2
0
2
max
tan
tanarctan
tantanarctan
1 2
Determination of Thickness
Interference fringes observed in the scattering pattern, due to different optical paths of the x-rays, are related to the thickness o