Model direct, reflected, and refracted arrivals using customizable Earth layers today quickly. Switch distance and velocity units, then download a clean record after solving.
| Scenario | Distance (km) | V1 (km/s) | V2 (km/s) | h (km) | Direct (s) | Reflected (s) | Refracted (s) |
|---|---|---|---|---|---|---|---|
| Direct only | 50 | 6.0 | — | — | 8.333 | — | — |
| Reflection | 50 | 6.0 | — | 20 | 8.333 | 10.034 | — |
| Two-layer | 50 | 6.0 | 8.0 | 20 | 8.333 | 10.034 | 7.532 |
Assumptions: horizontal layers, constant velocities in each layer, and a single planar interface.
In refraction surveys, the refracted arrival can become first at larger offsets. Compare direct and refracted times to estimate crossovers, then validate with observed picks.
For near-surface work, use realistic S-wave velocities (often 150–800 m/s) and consider strong heterogeneity. This tool intentionally keeps the physics transparent for quick checks.
Accurate travel times improve picks, inversions, and interpretations greatly.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.