Phase velocity

The phase velocity of a wave is the rate at which the wave propagates in some medium. This is the velocity at which the phase of any one frequency component of the wave travels. For such a component, any given phase of the wave (for example, the crest) will appear to travel at the phase velocity. The phase velocity is given in terms of the wavelength $λ$ (lambda) and time period $T$ as

v_{\mathrm {p} }={\frac {\lambda }{T}}.

Frequency dispersion in groups of gravity waves on the surface of deep water. The red square moves with the phase velocity, and the green circles propagate with the group velocity. In this deep-water case, the phase velocity is twice the group velocity. The red square overtakes two green circles when moving from the left to the right of the figure.

New waves seem to emerge at the back of a wave group, grow in amplitude until they are at the center of the group, and vanish at the wave group front.

For surface gravity waves, the water particle velocities are much smaller than the phase velocity, in most cases.

Propagation of a wave packet demonstrating a phase velocity greater than the group velocity without dispersion.

This shows a wave with the group velocity and phase velocity going in different directions. The group velocity is positive, while the phase velocity is negative.[1]

Equivalently, in terms of the wave's angular frequency $ω$ , which specifies angular change per unit of time, and wavenumber (or angular wave number) $k$ , which represents the proportionality between the angular frequency $ω$ and the linear speed (speed of propagation) ν_$p$,

v_{\mathrm {p} }={\frac {\omega }{k}}.

To understand where this equation comes from, consider a basic cosine wave, $A cos (kx - ωt)$ . After time $t$ , the source has produced $ωt/2 π = ft$ oscillations. After the same time, the initial wave front has propagated away from the source through space to the distance $x$ to fit the same number of oscillations, $kx = ωt$ .

Thus the propagation velocity v is $v = x / t = ω / k$ . The wave would have to propagate faster when higher frequency oscillations are distributed less densely in space unless the wave length is compensatorily shortened.[2] Formally, $Φ = kx - ωt$ is the phase, where

{\frac {\partial x}{\partial t}}=-{\frac {\partial \Phi /\partial t}{\partial \Phi /\partial x}}.

Since $ω = -d Φ /d t$ and $k = +d Φ /d x$ , the wave velocity is $v = d x /d t = ω / k$ .

Relation to group velocity, refractive index and transmission speed

A superposition of 1D plane waves (blue) each traveling at a different phase velocity (traced by blue dots) results in a Gaussian wave packet (red) that propagates at the group velocity (traced by the red line).

Since a pure sine wave cannot convey any information, some change in amplitude or frequency, known as modulation, is required. By combining two sines with slightly different frequencies and wavelengths,

{\begin{aligned}&\cos[(k-\Delta k)x-(\omega -\Delta \omega )t]\;+\;\cos[(k+\Delta k)x-(\omega +\Delta \omega )t]\\&=2\;\cos(\Delta kx-\Delta \omega t)\;\cos(kx-\omega t),\end{aligned}}

the amplitude becomes a sinusoid with phase speed $Δ ω /Δ k$ . It is this modulation that represents the signal content. Since each amplitude envelope contains a group of internal waves, this speed is usually called the group velocity, v_g.[2]

In a given medium, the frequency is some function $ω (k)$ of the wave number, so in general, the phase velocity $v p = ω / k$ and the group velocity $v g = d ω /d k$ depend on the frequency and on the medium. The ratio between the speed of light c and the phase velocity v_p is known as the refractive index, $n = c / v p = ck / ω$ .

Taking the derivative of $ω = ck / n$ with respect to $k$ , would yield the group velocity,

{\frac {{\text{d}}\omega }{{\text{d}}k}}={\frac {c}{n}}-{\frac {ck}{n^{2}}}\cdot {\frac {{\text{d}}n}{{\text{d}}k}}~.

except one cannot create a group with only a finite number of wave frequencies/wave vectors. (That is: the envelope in such a situation changes shape so rapidly that group velocity loses its meaning.) Noting that $c / n = v p$ , indicates that the group speed is equal to the phase speed only when the refractive index is a constant $d n /d k = 0$ , and in this case the phase speed and group speed are independent of frequency, $ω / k =d ω /d k = c / n$ .[2]

Otherwise, both the phase velocity and the group velocity vary with frequency, and the medium is called dispersive; the relation $ω = ω (k)$ is known as the dispersion relation of the medium.

The group velocity of electromagnetic radiation may – under certain circumstances (for example anomalous dispersion) – exceed the speed of light in a vacuum, but this does not indicate any superluminal information or energy transfer. It was theoretically described by physicists such as Arnold Sommerfeld and Léon Brillouin. See dispersion for a full discussion of wave velocities; however, the article fails to address the failure by such researchers to realize that in such cases the so-called index of refraction disobeys fundamental assumptions about such an object (see e.g. J.D.Jackson Classical Electrodynamics) so the "velocity" is not a group velocity at all.

References

Footnotes

Nemirovsky, Jonathan; Rechtsman, Mikael C; Segev, Mordechai (9 April 2012). "Negative radiation pressure and negative effective refractive index via dielectric birefringence" (PDF). Optics Express. 20 (8): 8907–8914. Bibcode:2012OExpr..20.8907N. doi:10.1364/OE.20.008907. PMID 22513601. Archived from the original (PDF) on 16 October 2013.
"Phase, Group, and Signal Velocity". Mathpages.com. Retrieved 2011-07-24.

Bibliography

Crawford jr., Frank S. (1968). Waves (Berkeley Physics Course, Vol. 3), McGraw-Hill, ISBN 978-0070048607 Free online version
Brillouin, Léon (1960), Wave Propagation And Group Velocity, New York and London: Academic Press Inc., ISBN 978-0-12-134968-4
Main, Iain G. (1988), Vibrations and Waves in Physics (2nd ed.), New York: Cambridge University Press, pp. 214–216, ISBN 978-0-521-27846-1
Tipler, Paul A.; Llewellyn, Ralph A. (2003), Modern Physics (4th ed.), New York: W. H. Freeman and Company, pp. 222–223, ISBN 978-0-7167-4345-3

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.

[nemirovsky2012negative-1] Nemirovsky, Jonathan; Rechtsman, Mikael C; Segev, Mordechai (9 April 2012). "Negative radiation pressure and negative effective refractive index via dielectric birefringence" (PDF). Optics Express. 20 (8): 8907–8914. Bibcode:2012OExpr..20.8907N. doi:10.1364/OE.20.008907. PMID 22513601. Archived from the original (PDF) on 16 October 2013.

[mathpages1-2] "Phase, Group, and Signal Velocity". Mathpages.com. Retrieved 2011-07-24.

Phase velocity

Relation to group velocity, refractive index and transmission speed

See also

References

Footnotes

Bibliography