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IWCS

Theory of heterogeneous viscoelasticity

, &
Pages 620-635 | Received 01 Sep 2015, Accepted 10 Nov 2015, Published online: 21 Dec 2015
 

Abstract

We review a new theory of viscoelasticity of a glass-forming viscous liquid near and below the glass transition. In our model, we assume that each point in the material has a specific viscosity, which varies randomly in space according to a fluctuating activation free energy. We include a Maxwellian elastic term, and assume that the corresponding shear modulus fluctuates as well with the same distribution as that of the activation barriers. The model is solved in coherent potential approximation, for which a derivation is given. The theory predicts an Arrhenius-type temperature dependence of the viscosity in the vanishing frequency limit, independent of the distribution of the activation barriers. The theory implies that this activation energy is generally different from that of a diffusing particle with the same barrier height distribution. If the distribution of activation barriers is assumed to have the Gaussian form, the finite-frequency version of the theory describes well the typical low-temperature alpha relaxation peak of glasses. Beta relaxation can be included by adding another Gaussian with centre at much lower energies than that is responsible for the alpha relaxation. At high frequencies, our theory reduces to the description of an elastic medium with spatially fluctuating elastic moduli (heterogeneous elasticity theory), which explains the occurrence of the boson peak-related vibrational anomalies of glasses.

Acknowledgements

W. S. is grateful for helpful discussions with U. Buchenau, J.C. Dyre, W. Götze, A. Loidel, T. Lunkenheimer, and R. Schilling.

Notes

No potential conflict of interest was reported by the authors.

1 We denote the Green’s function with a sans serif font in order to distinguish it from the shear modulus G.

2 At the end of the calculation, one has to take .

3 The Meyer–Neldel parameter need not be the same as that for the viscosity.

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