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We investigate the spatial dependence of the density of vibrated granular
beds, using simulations based on a hybrid Monte Carlo algorithm. We find that
the initial consolidation is typically inhmogeneous, both in the presence of a
constant shaking intensity and when the granular bed is submitted to annealed shaking'. We also present a theoretical model which explains such inhomogeneous relaxation in terms of a consolidation wave’, in good qualitative agreement
with our simulations. Our results are also in qualitative agreement with recent
simulations.

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