Thin-film interference 2026-10-18
Thin-film interference combines coherent light contributions reflected or transmitted at the two surfaces of a layer. For a film of refractive index , thickness and internal angle , the round-trip optical path difference is . The relative reflection phase shift must also be included. For a nonabsorbing higher-index film surrounded by air, one of the two leading reflected contributions has a phase shift and the other does not. Reflection maxima therefore satisfy . A smooth reflection spectrum filters many visible wavelengths at once; varying thickness and angle produce spatially varying mixed colours.
Model a thin transparent plate by a lossless reciprocal phase screen with transmission at the chosen angular frequency. Both passages multiply the local field by the same : reversing travel does not by itself change the sign of an accumulated optical path length. Assume the plate is stationary, the two passages use corresponding transverse positions, and the plate is adjacent to the return surface or perfectly reimaged onto it. Ignore propagation between these reference surfaces, wave absorption, clipping and intensity-dependent changes. Take the incident boundary envelope to be . Outward transmission gives . Ideal phase conjugation and the second transmission then give
This is a complete short proof of cancellation in the specified phase screen model. For an ideal ordinary mirror with constant reflection factor , the corresponding envelope is : the extra wave phase is , rather than zero. A constant reflection wave phase changes neither conclusion.
For an original toy optical aberration, let on , take , and choose
The even term adds symmetric curvature and the odd term makes the two sides unequal. The outward wave phase is ; immediately after ideal phase conjugation it is ; after the second passage it is zero. At , the outward values are , while an ordinary mirror's completed return has values . All wave phases here are unwrapped relative to the central ray and are otherwise equivalent modulo . At a stipulated vacuum wavelength , these outward errors correspond to optical path length errors of . These are chosen values; they are not observations or physical plate thicknesses.
Figure 1.
Original thin phase screen example: sign reversal at conjugation and cancellation after the second passage
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The wave phase plots make a subtle distinction visible: the field is still curved immediately after phase conjugation, and becomes flat only after crossing the same plate again. More generally, conjugation restores , not a universally flat wavefront. If the plate instead has transmission with real , the return is . Its plate-induced wave phase cancels but its lost wave amplitude does not recover. If the return plate has changed to wave phase , the residual factor is . Those two variations distinguish correction of a stationary optical aberration from universal reversal of loss or material evolution.
For an original classical calculation of the return step, neglect the residual ion's Coulomb force after release. Take a spatially uniform driving electric field , an Electron of electric charge and mass , and zero initial position and velocity at . With and , integrating Newton's second law gives
A return requires and . Define the cycle-averaged free-electron quiver kinetic energy
Searching the first-return solutions for release phases gives a maximum near and , with . For a chosen ionization energy , recombination into the initial state can therefore emit a photon with energy up to approximately in this model. This is an upper return-energy scale, not a prediction of the emitted yield. It omits release probabilities, quantum interference, propagation, phase matching and depletion of the neutral gas.
The calculation explains why a long driving wavelength can increase the available return energy: at fixed , grows as . It does not say that conversion efficiency improves. The Electron must return with a probability amplitude for emission that survives the microscopic dynamics and adds coherently across the gas.
Total hemispherical emissivity integrates over all emitted wavelengths and the outward hemisphere. If is spectral emissivity resolved by direction, and is blackbody spectral radiance from Planck's law, then
It is a weighted average, not an unweighted mean of surface properties. Even if the wavelength-resolved material response stays unchanged, the Planck's law weighting changes with temperature, so the total ratio can change. Likewise, total radiometric absorptance averaged over radiation from hotter surroundings generally differs from this emission-weighted ratio. Kirchhoff's law of thermal radiation equates matched spectral and directional quantities; it does not equate arbitrary broadband averages.
Total internal reflection Created 2026-09-29 Updated 2026-10-18
Total internal reflection occurs when a wave travels from higher to lower refractive index above the critical angle for total internal reflection, leaving no propagating transmitted plane electromagnetic wave normal to the interface.
At an infinite planar interface, total internal reflection returns all incident normal power in the reflected plane electromagnetic wave. Assume homogeneous dielectrics with isotropy, linearity, no dielectric loss, magnetic permeability , and positive real refractive indices . Above the critical angle for total internal reflection, both TE polarization and TM polarization have unit optical reflectance despite the external evanescent wave.[ref]
This makes total internal reflection useful for guiding light in an optical fiber: suitable internal incidence angles keep energy inside successive boundaries. Its more surprising feature is that perfect optical reflectance coexists with an external electric field. The evanescent field in total internal reflection can interact with a nearby object, as the frustrated total internal reflection experiment demonstrates.
For an original idealized example, choose , at vacuum wavelength . At angle of incidence , Snell law for electromagnetic waves gives an angle of refraction , so a transmitted light ray still emerges. At , its direction becomes tangent to the boundary. At , the proposed sine of a real angle of refraction would be : the transmitted wavevector must instead have an imaginary normal component. These are predictions for the stipulated media, not measured properties of a particular block.
Figure 1.
Constructed ray geometry just below, at, and above the critical angle for refractive indices 1.5 and 1; arrows indicate directions rather than relative powers
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A real semicircular-block experiment isolates this threshold. The University of Maryland laboratory instructions place a laser, motor-driven rotation stage and photodetector together; an aperture limits the detector voltage. The semicircular block is centered on the rotation axis, with the photodetector aligned along its flat face. The instructions identify a strong grazing-beam signal and a weaker signal just before the critical angle for total internal reflection. The readout is detector voltage versus stage angle. Retracing the incident laser beam identifies normal incidence for alignment.[ref]
The semicircular shape supplies a geometric control: a light ray passing radially through the curved face enters at normal incidence, avoiding additional entrance refraction. The weaker signal near the flat face locates a limiting angle of refraction; a vanishing remote-detector signal alone would not establish that the external electric field vanishes. Beam width and alignment limit angular resolution; no measured threshold or decay depth is supplied.[ref]
Transmittance 2026-10-14
Transmittance is the fraction of incident radiant flux transmitted through a specified object or boundary. Specify wavelength, angle of incidence, electromagnetic polarization and which outgoing light is collected.
Triple-axis spectrometer 2026-10-18
A triple-axis spectrometer uses Bragg's law at an initial crystal monochromator to select and at a second analyzing crystal to select . The sample sits between these selectors. The three axes refer to the monochromator, sample and analyzer rotations. The final counter measures accepted counts; the analyzer's wavelength selection makes those counts sensitive to outgoing energy even when the counter does not measure each neutron's energy directly.
Figure 1. . Original functional schematic, with illustrative bends rather than historical angles or distances. The upper route omits the analyzer; interpreting its peaks as elastic requires a physical assumption. The lower route selects both projectile energies. Neither route specifies a historical detector construction. Details.
For a constant- scan, change incident or outgoing energy while coordinating sample and analyzer settings so that stays fixed. Counts versus then probe excitations at one momentum transfer. Changing only the analyzer angle generally changes both transferred quantities. Incident-beam monitoring, analyzer response and the instrumental resolution must enter quantitative interpretation; the diagram's arrows specify information flow, not an absolute intensity calibration.
Add diffusivities to the basally forced quadratic activator-inhibitor model. A Fourier mode with has matrix and determinant . When , its trace is negative for every . A positive-growth mode therefore occurs precisely when for some positive . The parabola has a positive minimizer only if , and its minimum is negative exactly when . Thus the ordinary Turing instability requires , and . At onset, and the critical wavelength is . A bounded spatial domain further requires an allowed mode inside the unstable band.
Ultraviolet Created 2026-10-05 Updated 2026-10-14
Ultraviolet is electromagnetic radiation with wavelengths shorter than the violet end of ordinarily visible light. The CIE convention uses –, subdivided into UV-A at –, UV-B at – and UV-C at –. These divisions name intervals; they do not mark universal changes in every material's response. The boundary with visible light is not sharp, and other fields use near-, far-, vacuum- and extreme-ultraviolet divisions. [ref]. For example, NASA's Solar Dynamics Observatory observes extreme-ultraviolet bands below ; the CIE interval is therefore not the full extent of astronomical ultraviolet usage. [ref].
The CIE ultraviolet interval corresponds to frequencies about – and photon energies –, using vacuum wavelength and with Planck constant and speed of light . Shorter wavelength means larger energy per photon; larger irradiance means more incident power per area. These are different comparisons. At the same incident power, a ultraviolet beam has fewer photons per second than a infrared beam, even though each ultraviolet photon has more energy.
A common ultraviolet mechanism is photon absorption promoting an Electron from a ground state to an excited state of a chemical atom or molecule. By contrast, many infrared absorption bands involve stretching or bending chemical bonds. For either mechanism, both the energy difference and the coupling to the incident electromagnetic field matter. One concrete example is the absorption discussed for butadiene: an Electron moves between molecular orbitals, and the position of the absorption reveals their energy separation. Ultraviolet absorption can therefore probe molecular orbitals, while infrared spectroscopy probes many molecular motions. [ref].
Subsequent chemical reactions depend on the absorbing chemical substance and its environment; the label ultraviolet alone does not predict a reaction rate. At sufficiently short wavelength, a photon can cause photoionization if its energy exceeds the relevant ionization energy. There is no single wavelength that separates all ionizing from all nonionizing behavior for every chemical substance. Likewise, eventual heating after photon absorption is possible in both ultraviolet and infrared. The distinction is useful because different optical spectra expose different processes, not because the two ranges obey different laws of electromagnetism.
Ritter's 1801 observation used a chemical readout rather than a thermometer. In Caltech/IPAC's account, sunlight passed through a glass optical prism and silver chloride was placed in different parts of the optical spectrum. Darkening was weak toward red, stronger toward violet, and pronounced beyond the visible violet edge. The measured evidence was a change in the chemical substance's appearance at a spatial location with no visible color, establishing radiation beyond the eye's ordinary range. It was not a calibrated measurement of a universal ultraviolet optical spectrum. [ref].
A controlled modern interpretation of such a chemical test would compare equal exposure durations and matched fresh samples, keep an unexposed sample in darkness, monitor temperature, and distinguish scattered visible light from the intended short-wavelength beam with characterized filtering. These are proposed controls, not an assertion that Ritter performed them. Unequal sample preparation or heating can change a reaction rate. The optical prism, terrestrial atmosphere and sample response restrict which wavelengths the test detects. Darkening is a detector-weighted response, so its spatial maximum is not automatically the maximum of incoming radiant flux or of photon energy.
Thomas Larason and Jeanne Houston's NIST report documents a quantitative ultraviolet detector comparison. An argon source feeds a double-diffraction grating spectrometer; a shutter and mirrors deliver the selected band to a working-standard or test photodiode, successively at the same position. A beam splitter supplies a monitor photodiode. Amplifiers and voltmeters record detector and monitor simultaneously; shutter-closed readings provide dark baselines. The – scan, typically with bandpass, measures spectral responsivity. Monitor normalization suppresses source drift; known spectral lines calibrate wavelength. The report assesses temperature effects and unwanted light outside the band, weighted by detector response. The latter need not cancel between different spectral responsivities. [ref].
This determines electrical response without visual perception. Bandpass and spatial nonuniformity limit the calibration; aging and changed temperature can affect later use. The scan includes visible light and ultraviolet; no response below follows from it.
For a narrow beam, the idealized substitution calculation is
Here is spectral responsivity; and are dark-subtracted detector and monitor electric currents. This follows by writing for each detector and using the monitor to track changes in radiant flux. It assumes linear response, unchanged beam splitting and collection geometry, and a sufficiently narrow band. For an illustrative standard with , ratios and give . These invented arithmetic inputs illustrate the method; they are not NIST measurements.
An independent photon-counting model connects spectral responsivity to quantum efficiency. If is the number of collected Electrons per incident photon, there is no internal multiplication, and is the elementary charge, then
At illustrative constant and , this gives about at and at . The ultraviolet readout is smaller in this model because there are fewer incident photons, not because their individual energies are smaller. Real quantum efficiency depends on wavelength, windows, absorption and carrier collection; a detector's band gap and construction determine its usable range. Constant across these two wavelengths is an analytical comparison, not a claimed specification of a real photodiode.
Figure 1.
Photon energy across conventional ultraviolet and infrared ranges, with a schematic detector-substitution experiment
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The curve is the calculated relation , and the shaded ranges use the stated CIE conventions. The lower diagram abstracts the detector comparison rather than reproducing an instrument drawing. Together with the infrared heat-balance illustration, it shows why a calibrated detector response, rather than what looks bright to an observer, is the bridge between invisible radiation and a quantitative measurement.
Stipulate a distant circular source of uniform angular brightness, full angular diameter in radians, and narrow optical bandwidth around wavelength . Distinct source patches emit independently. Assume each collector is small enough not to resolve the disk individually. For a sky offset from the disk centre, the baseline-dependent phase difference is , up to channel-sign convention. Summing independent patch contributions makes the equal-delay first-order optical coherence the normalized Fourier transform of angular brightness:
Choose the horizontal coordinate along , put , and integrate along vertical chords of the disk:
The imaginary part cancels between opposite chords. Here is the order-one Bessel function of the first kind. One way to obtain the last equality is to integrate the exponential's power series term by term on the finite disk. Equivalently the result is specified by the convergent series
At take the continuous limit ; starts as . This is why very short interferometric baselines give little leverage on angular diameter. Larger disks lose spatial optical coherence at shorter baselines.
The first positive zero of is , so
This is a full diameter convention. The angle must be converted before substitution: one arcsecond is radians, and one milliarcsecond, abbreviated mas, is arcseconds. For the stipulated and , and . At , the model gives and .
Figure 1.
Stipulated uniform-disk model: signed field coherence, squared visibility and finite-gate intensity correlation versus interferometric baseline
. Original calculated curves for a 5-mas disk at 500 nm, with no measured points. The lower panel uses one polarization, independent signal fractions 0.8 in each channel, and the explicitly specified exponential temporal correlation and 50-ps gate below. It is not a fit to Sirius. Details.
Beyond , changes sign but stays nonnegative and develops weak further lobes. A single measured squared visibility can therefore match several angular diameters; sampling several interferometric baselines constrains the fit. Limb darkening, spectral averaging, or resolved collector apertures change the uniform-disk prediction. A uniform-disk diameter is a parameter of that brightness model; converting it to a physical stellar radius also requires distance and an appropriate brightness profile.
A monochromatic wave in vacuum has frequency and wavelength related by , where is the speed of light. During one oscillation period , a constant-wave phase surface travels one wavelength, so . Equivalently, the plane electromagnetic wave relation with angular frequency and wavenumber gives the same result.
As a calculated example, a vacuum radio wave with has using . Doubling frequency halves wavelength, independently of wave amplitude and wave intensity. The frequency spectrum of a pulse contains multiple frequencies; the relation applies to each vacuum component, rather than assigning one exact wavelength to the whole pulse. In a homogeneous medium replace by the appropriate phase velocity; the vacuum equation does not assert that all media have the same wavelength at a given frequency.