Ph.D. thesis (pdf) - dirac
Ph.D. thesis (pdf) - dirac
Ph.D. thesis (pdf) - dirac
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4.3. Inelastic Scattering Experiments 67<br />
is highly controversial and we shall not enter in this discussion. Suggestions are that<br />
it is due to disorder, fast relaxation or that it is a signature of the fact that the<br />
normal modes of the systems are not plane waves. [Ruocco et al., 2000; Ruffle et al.,<br />
2003; Matic et al., 2004]<br />
One of our main interest in the current study of the coherent dynamical structure<br />
factor is the nonergodicity factor. The nonergodicity factor is in principle the long<br />
time limit of the intermediate scattering function but it is operationally defined<br />
as the ratio of the central peak over the total coherent intensity. The intensity<br />
of the central peak is associated with the correlations that decay slower than the<br />
Brillouin frequency considered. It follows from equation 4.3.38 that this ratio in the<br />
hydrodynamic limit will be given by<br />
f q = 1 − v2 T<br />
vs<br />
2 . (4.3.43)<br />
The difference between the adiabatic and isothermal sound speeds is small in viscous<br />
liquids close to the glass transition. However, the relevant adiabatic sound speed<br />
is the sound speed at the Brillouin frequency, while the isothermal sound speed is<br />
the low frequency equilibrium sound speed. The generalization of this result in the<br />
viscoelastic liquid (still in the low Q limit) is therefore<br />
f q = 1 − v2 0<br />
v∞<br />
2 . (4.3.44)<br />
We apply this interpretation of the measured f Q in section 6.3.3.<br />
4.3.10 Long time limit and the resolution function<br />
The measured intensity in a scattering experiment includes a convolution with the<br />
experimental resolution function, R(ω). The delta function in equation 4.3.22 therefore<br />
becomes a broadened central peak in the experimental result<br />
∫ ∞<br />
S exp (Q, ω) = R(ω) ⊗ I ∞ (Q)δ(ω) + R(ω) ⊗ 1 I t (Q, t)exp(−iωt)dt<br />
2π −∞<br />
S exp (Q, ω) = R(ω)I ∞ (Q) + R(ω) ⊗ 1 ∫ ∞<br />
I t (Q, t)exp(−iωt)dt. (4.3.45)<br />
2π<br />
R(ω) is normalized and the long time limit of the intermediate scattering function,<br />
I ∞ (Q), can therefore be found from the integral over the central peak<br />
I ∞ (Q) =<br />
∫ ∆ω<br />
−∆ω<br />
−∞<br />
S exp (Q, ω)dω. (4.3.46)