Optical path length

In optics, optical path length (OPL, denoted ''Λ'' in equations), also known as optical length or optical distance, is the length that light needs to travel through a vacuum to create the same phase difference as it would have when traveling through a given medium. It is calculated by taking the product of the geometric length of the optical path followed by light and the refractive index of the homogeneous medium through which the light ray propagates; for inhomogeneous optical media, the product above is generalized as a path integral as part of the ray tracing procedure. A difference in OPL between two paths is often called the optical path difference (OPD). OPL and OPD are important because they determine the phase of the light and govern interference and diffraction of light as it propagates.

In a medium of constant refractive index, ''n'', the OPL for a path of geometrical length ''s'' is just

:$\mathrm = n s .\,$

If the refractive index varies along the path, the OPL is given by a line integral

:$\mathrm = \int_C n \mathrm ds,$

where ''n'' is the local refractive index as a function of distance along the path ''C''.

An electromagnetic wave propagating along a path ''C'' has the phase shift over ''C'' as if it was propagating a path in a vacuum, length of which, is equal to the optical path length of ''C''. Thus, if a wave is traveling through several different media, then the optical path length of each medium can be added to find the total optical path length. The optical path difference between the paths taken by two identical waves can then be used to find the phase change. Finally, using the phase change, the interference between the two waves can be calculated.

Fermat's principle states that the path light takes between two points is the path that has the minimum optical path length.

Optical path difference

The OPD corresponds to the phase shift undergone by the light emitted from two previously coherent sources when passed through mediums of different refractive indices. For example, a wave passing through air appears to travel a shorter distance than an identical wave traveling the same distance in glass. This is because a larger number of wavelengths fit in the same distance due to the higher refractive index of the glass.

The OPD can be calculated from the following equation:

:$\mathrm= d_1 n_1 - d_2 n_2$
where ''d''₁ and ''d''₂ are the distances of the ray passing through medium 1 or 2, ''n''₁ is the greater refractive index (e.g., glass) and ''n''₂ is the smaller refractive index (e.g., air).

See also

* Air mass (astronomy)
* Lagrangian optics
* Hamiltonian optics
*Fermat's principle
* Optical depth

References

*
*{{cite book , last = Jenkins , first = F. , author2=White, H. , title = ''Fundamentals of Optics'' , url = https://archive.org/details/fundamentalsofop0004jenk , url-access = registration , edition = 4th , publisher = McGraw-Hill , year = 1976 , isbn = 0-07-032330-5

Geometrical optics
Physical optics
Optical quantities