In the , the wavenumber (or wave number), also known as repetency, is the spatial frequency of a wave. Ordinary wavenumber is defined as the number of divided by length; it is a physical quantity with dimension of reciprocal length, expressed in SI units of cycles per metre or reciprocal metre (m−1). Angular wavenumber, defined as the wave phase divided by time, is a quantity with dimension of angle per length and SI units of per metre. They are analogous to temporal frequency, respectively the ordinary frequency, defined as the number of wave cycles divided by time (in cycles per second or reciprocal seconds), and the angular frequency, defined as the phase angle divided by time (in radians per second).
In multidimensional systems, the wavenumber is the magnitude of the wave vector. The space of wave vectors is called reciprocal space. Wave numbers and wave vectors play an essential role in optics and the physics of wave scattering, such as X-ray diffraction, neutron diffraction, electron diffraction, and elementary particle physics. For quantum mechanical waves, the wavenumber multiplied by the reduced Planck constant is the canonical momentum.
Wavenumber can be used to specify quantities other than spatial frequency. For example, in optical spectroscopy, it is often used as a unit of temporal frequency assuming a certain speed of light.
Definition
Wavenumber, as used in
spectroscopy and most chemistry fields,
is defined as the number of
per unit distance:
where
λ is the wavelength. It is sometimes called the "spectroscopic wavenumber".
It equals the spatial frequency.
In theoretical physics, an angular wave number, defined as the number of radians per unit distance is more often used:
- .
Units
The SI unit of spectroscopic wavenumber is the reciprocal m, written m
−1.
However, it is more common, especially in
spectroscopy, to give wavenumbers in
cgs units i.e., reciprocal centimeters or cm
−1, with
- .
Occasionally in older references, the unit kayser (after Heinrich Kayser) is used; it is abbreviated as K or Ky, where 1K = 1cm−1.
Angular wavenumber may be expressed in the unit radian per meter (rad⋅m−1), or as above, since the radian is dimensionless.
Unit conversions
The frequency of light with wavenumber
is
- ,
where
is the speed of light.
The conversion from spectroscopic wavenumber to frequency is therefore
Wavenumber can also be used as unit of energy, since a photon of frequency has energy , where is the Planck constant.
The energy of a photon with wavenumber is
- .
The conversion from spectroscopic wavenumber to energy is therefore
= 1.986446 \times 10^{-23}~\mathrm{J}
= 1.239842 \times 10^{-4}~\mathrm{eV}
where energy is expressed either in
Joule or
Electronvolt.
Complex
A complex-valued wavenumber can be defined for a medium with complex-valued relative
permittivity , relative permeability
and
refraction index n as:
[[1], eq.(2.13.3)]
where
k0 is the free-space wavenumber, as above. The imaginary part of the wavenumber expresses attenuation per unit distance and is useful in the study of exponentially decaying
.
Plane waves in linear media
The propagation factor of a sinusoidal plane wave propagating in the positive x direction in a linear material is given by
where
-
-
phase constant in the units of /meter
-
attenuation constant in the units of /meter
-
angular frequency
-
distance traveled in the x direction
-
conductivity in Siemens/meter
-
complex permittivity
-
complex permeability
-
The sign convention is chosen for consistency with propagation in lossy media. If the attenuation constant is positive, then the wave amplitude decreases as the wave propagates in the x-direction.
Wavelength, phase velocity, and skin effect have simple relationships to the components of the wavenumber:
In wave equations
Here we assume that the wave is regular in the sense that the different quantities describing the wave such as the wavelength, frequency and thus the wavenumber are constants. See
wavepacket for discussion of the case when these quantities are not constant.
In general, the angular wavenumber k (i.e. the magnitude of the wave vector) is given by
where
ν is the frequency of the wave,
λ is the wavelength,
ω = 2
πν is the angular frequency of the wave, and
vp is the
phase velocity of the wave. The dependence of the wavenumber on the frequency (or more commonly the frequency on the wavenumber) is known as a dispersion relation.
For the special case of an electromagnetic wave in a vacuum, in which the wave propagates at the speed of light, k is given by:
where
E is the
energy of the wave,
ħ is the reduced Planck constant, and
c is the speed of light in a vacuum.
For the special case of a matter wave, for example an electron wave, in the non-relativistic approximation (in the case of a free particle, that is, the particle has no potential energy):
Here
p is the
momentum of the particle,
m is the
mass of the particle,
E is the
kinetic energy of the particle, and
ħ is the reduced Planck constant.
Wavenumber is also used to define the group velocity.
In spectroscopy
In
spectroscopy, "wavenumber"
(in
Reciprocal meter, cm
−1) refers to a temporal frequency (in hertz) divided by the speed of light in vacuum (usually in centimeters per second, cm⋅s
−1):
The historical reason for using this spectroscopic wavenumber rather than frequency is that it is a convenient unit when studying atomic spectra by counting fringes per cm with an
interferometer : the spectroscopic wavenumber is the reciprocal of the wavelength of light in vacuum:
which remains essentially the same in air, and so the spectroscopic wavenumber is directly related to the angles of light scattered from diffraction gratings and the distance between fringes in
, when those instruments are operated in air or vacuum. Such wavenumbers were first used in the calculations of
Johannes Rydberg in the 1880s. The Rydberg–Ritz combination principle of 1908 was also formulated in terms of wavenumbers. A few years later spectral lines could be understood in quantum theory as differences between energy levels, energy being proportional to wavenumber, or frequency. However, spectroscopic data kept being tabulated in terms of spectroscopic wavenumber rather than frequency or energy.
For example, the spectroscopic wavenumbers of the emission spectrum of atomic hydrogen are given by the Rydberg formula:
where
R is the
Rydberg constant, and
ni and
nf are the principal quantum numbers of the initial and final levels respectively (
ni is greater than
nf for emission).
A spectroscopic wavenumber can be converted into photon energy E by Planck's relation:
It can also be converted into wavelength of light:
where
n is the
refractive index of the
optical medium. Note that the wavelength of light changes as it passes through different media, however, the spectroscopic wavenumber (i.e., frequency) remains constant.
Often spatial frequencies are stated by some authors "in wavenumbers",[See for example,
] incorrectly transferring the name of the quantity to the CGS unit cm−1 itself.[
]
See also
External links