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Diploma Thesis - Erich Schmid Institute

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d<br />

ϕψ<br />

ϕψ,<br />

hkl,<br />

R<br />

= d (1+<br />

( x ε + ( 1−<br />

x)<br />

ε<br />

0<br />

33<br />

Polycrystalline and monocrystalline Model<br />

ϕψ,<br />

V<br />

33<br />

Equation 7.11 will be used for nonlinear regression and d0 is substituted by:<br />

d<br />

ϕψ<br />

a 0 ϕψ,<br />

hkl,<br />

R<br />

ϕψ,<br />

V<br />

= (1+<br />

( x ε33<br />

+ ( 1−<br />

x)<br />

ε33<br />

)) (equ 7.11)<br />

2 2 2<br />

h + k + l<br />

7.2. Calculating stresses for a single crystalline material<br />

The examination of isotropic polycrystalline material differs from anisotropic single<br />

crystalline material in such a way that an untextured polycrystalline material fulfils the<br />

Bragg condition at every ψ-ϕ tilt because there are always crystals with net plane<br />

normals parallel to the measuring direction in the laboratory system. However Bragg<br />

reflections of single crystals can only be detected at strict defined tilts [24].<br />

ε = O O O O s σ<br />

(equ 7.12)<br />

ij<br />

e<br />

mi<br />

e<br />

nj<br />

e<br />

ok<br />

Only strains can be measured, hence the stresses must be expressed with a linear<br />

elastic anisotropic material model. The strains in the sample system are depending<br />

on the crystal position therefore the orthogonal tensor O e , which is described by Euler<br />

angles, is introduced to express the relation between the sample and the crystal<br />

system.<br />

ij<br />

D<br />

ki<br />

e<br />

pl<br />

D<br />

lj<br />

kl<br />

mnop<br />

kl<br />

))<br />

ε = O O ε<br />

ϕω (equ 7.13)<br />

The strain measurement is done in the laboratory system, so the sample’s tilt is<br />

defined by equation 7.13 which is similar to equation 7.6 except that the strain tensor<br />

is rotated and ω−angle is used instead of ψ.<br />

In the case of gallium nitride and gallium boron nitride on sapphire the basal plane of<br />

the GaN crystal and BGaN crystal is perpendicular to the surface normal, so further<br />

calculations are simplified in such a way that no orthogonal tensor O e is needed,<br />

because of the transversal isotropy of the hexagonal lattice.<br />

ε = O O s σ<br />

ϕω (equ 7.14)<br />

33<br />

D<br />

i3<br />

D<br />

j3<br />

ijkl<br />

kl<br />

29

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