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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 23 (2001), S. 365-372 
    ISSN: 1434-6036
    Keywords: PACS. 05.45.Mt Semiclassical chaos (“quantum chaos") – 46.40.-f Vibrations and mechanical waves
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract: We report a numerical study of the flexural modes of a plate using semi-classical analysis developed in the context of quantum systems. We first introduce the Clover billiard as a paradigm for a system inside which rays exhibit stable and chaotic trajectories. The resulting phase space explored by the ray trajectories is illustrated using the Poincare surface of section, and shows that it has both integrable and chaotic regions. Examples of the stable and the unstable periodic orbits in the geometry are presented. We numerically solve the biharmonic equation for the flexural vibrations of the Clover shaped plate with clamped boundary conditions. The first few hundred eigenvalues and the eigenfunctions are obtained using a boundary elements method. The Fourier transform of the eigenvalues show strong peaks which correspond to ray periodic orbits. However, the peaks corresponding to the shortest stable periodic orbits are not stronger than the peaks associated with unstable periodic orbits. We also perform statistics on the obtained eigenvalues and the eigenfunctions. The eigenvalue spacing distribution P(s) shows a strong peak and therefore deviates from both the Poisson and the Wigner distribution of random matrix theory at small spacings because of the C4v symmetry of the Clover geometry. The density distribution of the eigenfunctions is observed to agree with the Porter-Thomas distribution of random matrix theory.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © Europhysics Letters Association, 2012. This is the author's version of the work. It is posted here by permission of Europhysics Letters Association for personal use, not for redistribution. The definitive version was published in EPL (Europhysics Letters) 98 (2012): 58003, doi:10.1209/0295-5075/98/58003.
    Description: Flow through a saturated, granular, porous medium can lead to internal erosion, preferential flow enhancement and the formation of channels within the bulk of the medium. We examine this phenomenon using a combination of experimental observations, continuum theory and numerical simulations in a minimal setting. Our experiments are carried out by forcing water through a Hele-Shaw cell packed with bidisperse grains. When the local fluid flow-induced stress exceeds a critical threshold, the smaller grains are dislodged and transported, thus changing the porosity of the medium and thence the local hydraulic conductivity and the development of erosional channels. The erosion is ultimately arrested due to the drop in the mean pressure gradient, while most of the flow occurs through the channels. These observations are consistent with a simple theoretical model for channelization in terms of a macroscopic multiphase description of erosion. We model a dynamical porosity field that evolves along with the volume fraction of the mobile and immobile grains in response to fluid flow. Numerical solutions of the resulting initial boundary value problem yield results for the dynamics and morphology that are in qualitative agreement with our experiments. In addition to providing a basis for channelization in porous media, our study highlights how heterogeneity in porous media may arise from flow as a function of the erosion threshold, and thus potentially offers the ability to control channelization.
    Description: We thank DOE NICCR (AM, AK), Harvard-NSF MRSEC (LM) and the MacArthur Foundation for partial support.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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