Permanent Displacement Response Spectra
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Critical field parameters in compliant dynamic displacement analysis:
(a) Shear wave velocity measurements characterize soil stiffness and resonance |
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| Shear wave velocity profiles are determined by the Spectral Analysis of Surface Waves (SASW) method. Field motion data are collected and a Rayleigh wave dispersion curve is computed. The shear wave profile is computed by forward inversion. | |
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(b) Soil yielding stress is determined by shearing the soil. For clay deposits we use a large self-boring vane apparatus that sounds to 10 meters. |
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We visited sites throughout San Francisco Bay to measure the shear resistance of soft Bay Mud. We found that the effective stress normalized shear strength properties are similar, regardless of location. |
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Click on figures to view larger image (32K) (16K). | |
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last modified 1 December 2003 (lzt)
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Department of the Interior U.S. Geological Survey Geologic Division Coastal & Marine Geology Program Western Region Coastal & Marine Geology