Seismic refraction methods are geophysical exploration techniques that use the travel times of compressional or shear waves refracted at subsurface interfaces to infer the velocity structure and geometry of geological layers. Controlled seismic sources generate wavefronts that critically refract along higher-velocity layers and return energy to surface receivers at characteristic distances, producing refracted arrivals whose travel-time curves are analyzed. By interpreting these curves using ray theory, inversion algorithms, and layered or gradient velocity models, seismic refraction enables quantitative estimation of layer thicknesses, seismic velocities, and structural discontinuities, particularly in near-surface investigations for engineering, hydrogeological, and shallow crustal studies.
Science never stops. Get notified about trending stories.
