Stress response function of a granular layer: quantitative comparison between experiments and isotropic elasticity
We measured the vertical pressure response function of a layer of sand submitted to a localized normal force at its surface. We found that this response profile depends on the way the layer has been prepared: all profiles show a single centered peak whose width scales with the thickness of the layer...
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Main Authors: | , , , , |
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Format: | Journal Article |
Language: | English |
Published: |
31-07-2001
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Subjects: | |
Online Access: | Get full text |
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Summary: | We measured the vertical pressure response function of a layer of sand
submitted to a localized normal force at its surface. We found that this
response profile depends on the way the layer has been prepared: all profiles
show a single centered peak whose width scales with the thickness of the layer,
but a dense packing gives a wider peak than a loose one. We calculate the
prediction of isotropic elastic theory in presence of a bottom boundary and
compare it to the data. We found that the theory gives the right scaling and
the correct qualitative shape, but fails to really fit the data. |
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DOI: | 10.48550/arxiv.cond-mat/0107626 |