Downhole Seismic Test
Downhole seismic testing is a geophysical method used to measure the seismic wave velocities (P-wave and S-wave) of subsurface materials at different depths. This test is crucial for site-specific seismic design, ground response analysis, and soil classification in accordance with international codes. The process involves placing geophones in a borehole and generating seismic waves at the surface to record their travel times through soil and rock layers. The data helps determine dynamic soil properties needed for earthquake-resistant structural design.
Key aspects include:
- Measures P-wave (compressional) and S-wave (shear) velocities
- Performed using a vertical borehole with downhole geophones
- Supports seismic site classification (e.g., as per Eurocode 8, IBC)
- Determines soil stiffness and dynamic properties
- Essential for ground response and liquefaction analysis
- Accurate, depth-specific data for seismic and geotechnical design