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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)

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