Nonlinear sound propagation in a stressed glass bead pack is investigated via amplitude measurements of harmonic generation. We evidence two distinct regimes of sound-matter interaction: reversible and irreversible, as a function of the ratio rs between dynamic strain and static one. In the reversible regime, the higher harmonics generated agree well with a mean-field model based on the Hertz contact theory, and the coefficient of nonlinearity β deduced from the measured amplitude of second-harmonic is consistent with that deduced from the acoustoelastic measurement. Beyond a certain threshold (rs > 3%), the interaction of sound wave with granular matter becomes irreversible, accompanied by a small compaction of the medium. Copyright 2008 by the American Geophysical Union.
CITATION STYLE
Brunet, T., Jia, X., & Johnson, P. A. (2008). Transitional nonlinear elastic behaviour in dense granular media. Geophysical Research Letters, 35(19). https://doi.org/10.1029/2008GL035264
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