wave velocity

Therefore, the wave velocity will decrease with added mass.

The P wave velocity in the north is 7% slower than that in the south.

Group velocity is often considered to be the wave velocity at which information travels.

The wave velocity helped his speed and in another few moments he stood atop the next crest but could see no farther.

See dispersion for a full discussion of wave velocities.

A large scale (100 m) have shown a significant increase in shear wave velocity was observed during the treatment.

Shaking is stronger where the shear wave velocity is lower.

There are a number of methods used to determine a site's shear wave velocity:

To reduce drag, superluminal wave velocities were necessary, and they would still be subject to the heating problem.

By measuring a soil's shear wave velocity, the dynamic response of that soil can be estimated.

Wave velocity is a wave property, which may refer to:

It then converges, from above, to the Rayleigh wave velocity in the high frequency limit.

If the seismic wave velocity in the rock is known, then the travel time may be used to estimate the depth to the reflector.

Consequently, wavelength, period, and wave velocity are related just as for a traveling wave.

The dependence of wave velocity on frequency or wavelength:

They usually travel slightly faster than Rayleigh waves, about 90% of the surface wave velocity, and have the largest amplitude.

Information travels at the wave velocity.

Calculations of frequency and wave velocity of motility could be derived directly from the screen.

The boundary is observed via the discontinuity in seismic wave velocities at that depth.

The waves of energy are P-waves generated by earthquakes and are recording the wave velocities.

More detailed information on the shear wave velocity profile of the site can be obtained from microtremor array observation.

Supershear - rupture propagates faster than seismic shear wave velocity.

It is characterized by unusually low seismic shear wave velocity compared to the surrounding depth intervals.

The standard data processing of sonic logs to derive wave velocity and energy content is explained in and.

Instead the change in the seismic wave velocity is caused by a metamorphic transition in the granite rock.