Abstract
Shear-wave velocity measured by bender elements in laboratory sand samples is shown to be dependent upon the excitation frequency and exhibits a maximum velocity for a finite frequency. By comparing the relative effects of dispersion due to propagation of shear waves through sand and dispersion due to bender element performance within sand, we show that a combination of the two processes is required to explain the observations. The magnitude of the aggregate response of the bender elements and the sand implies that reliable shear-wave velocity results cannot be obtained from bender element tests without a prior knowledge of the frequency response of the entire system.
| Original language | English |
|---|---|
| Pages (from-to) | 1348-1357 |
| Number of pages | 10 |
| Journal | Canadian Geotechnical Journal |
| Volume | 37 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 2000 |
Keywords
- Attenuation
- Dispersion
- Phase-sensitive detection
- Sand
- Shear-wave velocity
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