Refraction Created 2026-10-13 Updated 2026-10-14
Refraction changes the direction of a transmitted wave when it crosses between media with different phase velocities. For light at a planar interface, Snell's law relates the angles measured from the normal vector through the refractive indices. At normal incidence the direction remains unchanged even though the wavelength and phase velocity can change. The worked example under geometrical optics distinguishes transmission from total internal reflection.
For light, refraction explains why a submerged object looks nearer the surface and why an optical lens can form an image. A wavefront crossing a boundary must retain a consistent wave phase along that boundary: its normal spacing changes with phase velocity, and oblique light rays change direction. Normal incidence separates these two effects especially clearly.
Take stationary, transparent, homogeneous media with isotropy, linearity of their optical response, and real positive refractive indices, at one chosen frequency . With the vacuum speed of light and the vacuum wavelength, medium has
The frequency is unchanged at a stationary boundary; the phase velocity, wavelength and wavenumber can change. Here is a phase refractive index, not the group refractive index. If there is optical dispersion, evaluate at this same frequency on both sides.[ref]
For an original idealized air–water example, stipulate and , with vacuum wavelength . Then , the water phase velocity is , and its wavelength is . At an air angle of incidence , Snell's law gives a water angle of refraction . These stipulated values illustrate the relations; actual refractive indices depend on material conditions and frequency. By reversibility of an optical ray, the same path emerging from water has outgoing air angle .
Refractive index Created 2026-09-29 Updated 2026-10-18
The refractive index compares the phase velocity of light in a medium with the vacuum speed of light . For a transparent, uniform medium with isotropy and a positive-index propagation branch,
Here is the angular frequency, is the wavenumber, and is the speed of a surface of constant wave phase. The refractive index is a dimensionless quantity; it is a property of a specified material response at a specified frequency, rather than a universal number attached to the word “glass”. More general absorbing or negative-index media require the conventions discussed in refractive index and electromagnetic response. [ref]
For an original model example, choose at vacuum wavelength . The phase velocity is , the frequency is , and the medium wavelength is . These are stipulated model values, not measured properties of glass or water. A value at this single frequency does not determine a pulse's group velocity.
The usefulness of refractive index is that one measured response connects several different observations: Snell's law predicts refraction, optical path length predicts accumulated wave phase, and changes with frequency describe optical dispersion. Even at normal incidence, where a light ray does not bend, a changed refractive index changes wavelength and wave phase. The following comparison isolates that effect; the oblique geometry is developed in wavefront.
Figure 1.
Chosen refractive index : shorter wavelength, slower wavefronts, unchanged interface frequency
. The top panel compares equal normalized electric field components at one time on either side of a stationary interface at normal incidence. The lower panel tracks constant-wave phase crests in space and time. Curves represent incident and transmitted components, with their amplitudes normalized separately; reflected light and interface amplitude matching are omitted. The chosen single-frequency model contains no measured material data. Details.
For a linear stationary interface, phase matching at a planar wave interface preserves frequency: the incident and transmitted electric fields must oscillate together at each boundary point. Their phase velocities can differ, so their wavelengths differ. Writing , the definitions give
This explains the compressed wavefront spacing in the figure without changing the time between crests at the interface. Moving interfaces or time-dependent material responses need not preserve frequency. [ref]
The notation labels refractive index by vacuum wavelength; it does not mean the wavelength inside the material. Dependence on , equivalently on frequency, is optical dispersion. The field driving the material induces oscillating electric charges; their emitted electromagnetic fields combine with the applied field to change the resulting wave phase. This collective response motivates refractive index, rather than a picture of independently delayed little pieces of light. [ref]
To distinguish three speeds, track a wavefront for phase velocity, a narrow wave envelope for group velocity, and the earliest newly introduced disturbance for front velocity. For a transparent differentiable propagation branch,
The denominator is the group refractive index. It describes envelope transit when loss and reshaping are small. It need not equal , and neither phase velocity nor a reshaped pulse peak generally measures signal arrival. The front velocity article explains the separate relativistic causality constraint and why a detector threshold is not an exact causal-front measurement.
For two lines measured with the same interplanar spacing at the same temperature, division of Bragg's law gives
The common cancels. Consequently a precise wavelength ratio can coexist with an uncertain conversion to SI length. In contrast, angular calibration errors generally survive: a shared small zero offset changes the inferred ratio fractionally by approximately . Nearby lines partially cancel this effect, but widely separated angles need not. Different crystals, temperatures or refraction corrections also prevent unqualified cancellation.
Relativistic Doppler effect Created 2026-10-07 Updated 2026-10-18
The Lorentz transformation changes the photon four-momentum and therefore its frequency, producing the displayed formula for a boost along the first axis. Here the primed ray angle is measured in the emitting frame and . The angle and frequency transforms must be used together: aberration of light changes the direction, and a photon-number angular fraction need not equal the corresponding radiant-energy fraction.
Here is the vacuum speed of light, is the Lorentz factor, and the two frequencies are measured in different inertial reference frames. Unlike the classical Doppler effect for sound, there is no material rest reference frame for light in vacuum. For small radial recession speed , the wavelength shift satisfies . This small-speed limit underlies Doppler spectroscopy; it is not an exact sound formula.
A freely moving rod end has zero axial stress, not zero axial displacement. For a uniform slender rod of length , its low-frequency extensional modes have shapes and wavelengths . A centre clamp is compatible with the displacement node and ; clamps at and are compatible with and . The support positions therefore matter before a gas wavelength can determine a rod speed of sound.
For a chosen model with , and , the slender-rod extensional relation gives . The two-quarter-support mode then has . If the gas has stipulated , its half-wavelength is , and
The centre-supported fundamental would instead have and twice that gas spacing. The same rod material has not changed its wave speed. In this slender-rod model, is Young's modulus; a bulk compressional wave involves a different elastic-modulus combination, so the two wave speeds are not interchangeable.
Ruby pressure scale 2026-10-18
The ruby pressure scale converts a shift of a ruby fluorescence spectral line into pressure. Excitation light produces a fluorescence emission spectrum; fitting its line gives a wavelength . The reference must be measured or assigned at specified reference pressure and temperature. The difference is an observable; interpreting it as pressure requires a pressure calibration and suitable stress conditions.
The original 1972 report found sharp emission shifting toward lower photon energy as pressure increased; it tentatively associated broadening with nonhydrostatic conditions.[ref] In use, excitation rejection, a calibrated wavelength axis and a fitted background matter because leakage or background can move an apparent peak. A brighter trace improves counting statistics but does not alone establish a correct pressure scale.
Construct a synthetic local calibration to show the calculation independently of the historical data. Choose reference pairs , with shifts in and pressures in . The reference zero is already subtracted. Treat the shifts as exact for this fit and give the three reference pressures equal weights. Minimizing the ordinary least squares objective
and setting its derivative to zero gives
The regression residuals are . Their weighted moment vanishes, as required by the least-squares normal equations. An unknown reference offset requires fitting an intercept instead; forcing it to zero can bias the slope. If shift errors matter, this elementary fit is insufficient.
Figure 1.
Synthetic ruby pressure scale: fitting the response and propagating measurement uncertainty
. Original stipulated reference points and calculations, not measured historical calibration. The left panel shows the fitted slope and a chosen reading. The right panel separates independent contributions to standard uncertainty; bar lengths are standard contributions, which combine by sums of squares. The assigned slope standard uncertainty includes a hypothetical reference-scale contribution and is not estimated from the three residuals. Details.
Use the local measurement model
Here denotes pressure relative to the reference, is calibrated sensitivity, and is a local wavelength sensitivity to temperature at fixed pressure. Choose , and a reading at . The inferred pressure is . These coefficients and readings are stipulated, not measured ruby constants. With the same pressure, a increase in temperature would add to the shift in this model; neglecting it would overestimate pressure by .
Assign independent standard uncertainties , and for the temperature difference. Here is an independently assigned calibration uncertainty, not an estimate from the regression residuals above; treat as exact in this example. First-order propagation of uncertainty follows by differentiating the measurement model:
The four standard contributions are , giving . This is a standard uncertainty, not automatically a interval. Correlated reference and loaded wavelength readings require the corresponding covariance term; common wavelength-axis drift may cancel in their difference. Uncertain , nonzero , model inadequacy and unresolved deviatoric stress require a broader budget. Taking more optical readings reduces some random errors while leaving a common reference-scale error.
Ruby R-line shift 2026-10-18
The ruby R-line shift compares the same emission feature under two conditions. It is distinct from the Stokes shift, which compares absorption and emission features. In ruby, chromium ions in the corundum crystal provide the electronic transitions; compression changes their local environment and transition energies.[ref]
For consistently defined vacuum wavelengths, the reciprocal relation gives
Thus a positive wavelength shift means a negative reciprocal shift, and gives lower photon energy; is the Planck constant and the speed of light. For spectroscopic wavenumber, use vacuum wavelength and keep that convention consistent. A calibration specified in air wavelength must retain its convention or be converted consistently. The reciprocal relation is nonlinear: a line exactly linear in is not exactly linear in .
For a purely mathematical check with chosen vacuum wavelengths and , the reciprocal shift is . The small-shift approximation gives , about too large in magnitude. These chosen values illustrate the conversion; they are not measured ruby lines or an additional pressure calibration.