Rayleigh scattering by a small sphere Created 2026-10-14 Updated 2026-10-20
Consider a fixed, homogeneous, nonabsorbing, nonmagnetic sphere of radius in vacuum. Let be its relative refractive index, a fixed real number; in vacuum this equals the sphere's refractive index. Treat as independent of wavelength over the range being compared, neglecting optical dispersion. Air can be approximated by vacuum here because its refractive index is close to one. These assumptions describe a toy particle, rather than a literal model of an individual air molecule.
The Rayleigh scattering cross-section is an effective area: the total scattered power is , where is the incident light intensity. For its leading approximation is
The units are area, since has units . This Rayleigh scattering cross-section measures scattering, not conversion of the incident electromagnetic radiation into heat. The definition follows [ref].
To see the mechanism, the nearly uniform applied electric field produces an electric dipole moment with peak magnitude
where is the incident electric field peak wave amplitude and is vacuum permittivity. This is the sphere's response in electrostatics, with its permittivity divided by vacuum permittivity equal to under the nonmagnetic assumption. [ref]. The averaged electric dipole radiation power is , with angular frequency and speed of light . Dividing by gives the displayed Rayleigh scattering cross-section. Thus doubling radius multiplies the electric dipole moment by eight and the scattered power by , provided the larger sphere still satisfies . [ref].
A tube of neighboring elastic rays follows the wavefront normal. If is its infinitesimal transverse area, its expansion is along arclength. The P-wavefront discontinuity transport law therefore gives the displayed conserved flux. Geometrical spreading, mass density and wave speed determine the leading jump wave amplitude together; the rule is valid before the ray tube reaches a caustic.
For a uniform linear medium with isotropy and local constitutive response, Maxwell equations give . Here is permittivity and is magnetic permeability. Since , the relative permittivity and the relative magnetic permeability obey
If both responses are real and positive with negligible loss, and the ordinary positive-index branch is intended, then . If additionally , then . All these responses must be evaluated at the electromagnetic wave's frequency; a static relative permittivity cannot simply be substituted at an optical frequency. [ref]
With loss, use a complex index and explicitly fix the phase convention for complex amplitudes. For with , its wave amplitude has factor . A forward attenuating branch has , while its wave phase is controlled by . The complex relation alone leaves a choice of sign: the physical solution also needs causality and the appropriate radiation or decay condition. In negative-index media the physically selected real part can be negative. The positive square root is therefore not a universal rule for complex or negative-index media. Direction and polarization of an electromagnetic wave also matter in a plane wave in an anisotropic dielectric, for which one scalar index need not describe every propagation branch.
Reverberation time Created 2026-10-18 Updated 2026-10-24
The conventional reverberation time is the time for the level of decaying acoustic energy to decrease by decibels, a factor in energy or in pressure wave amplitude. For exponential energy decay , . It is not the exponential relaxation time itself and cannot be inferred exactly from an unspecified audibility threshold.
Scalar wave intensity Created 2026-10-13 Updated 2026-10-14
For a scalar complex wave amplitude , the squared-amplitude scalar wave intensity convention is . It is nonnegative and unchanged by multiplying by a unit-modulus wave phase factor. This convention is useful in paraxial propagation and phase screen models. Conversion to physical energy flux also depends on the field variable and medium; an arbitrary superposition need not have its full flux determined by this scalar alone. For a random field, is the mean wave intensity, whereas is the squared coherent field; these generally differ.
SH ray-tube amplitude transport Created 2026-10-14 Updated 2026-10-20
For a leading wavefront singularity or discontinuity in a smooth isotropic shear-horizontal wave field, the ray transport equation conserves the displayed quantity along a tube of elastic rays. Here is transverse tube width in two dimensions and area in three. Cylindrical spreading has , so the leading wave amplitude is proportional to . This rule excludes the immediate source neighborhood and caustics.
Single-slit diffraction Created 2026-10-14 Updated 2026-10-18
Single-slit diffraction is the spreading of light transmitted by one slit. Consider an ideal rectangular slit of width , illuminated normally by a uniform plane wave with a single wavelength in the surrounding medium. This monochromatic wave has uniform wave amplitude and equal incident wave phases across the slit, providing the required optical coherence. In the scalar Fraunhofer diffraction model, the normalized angular wave intensity is
Here is measured from the forward normal in the plane across the slit width. The sinc function uses the unnormalized convention . The limit makes the central value one. This ideal envelope neglects additional direction-dependent propagation and detector factors; near the forward direction it describes the normalized screen irradiance. [ref].
The noncentral zeros satisfy
The restriction follows from the range of the sine of a real angle. The first minima have when . If , this model has no noncentral zero in the forward hemisphere; equality puts the first zeros at grazing directions, outside the small-angle approximation and off any finite perpendicular screen. [ref].
For , define the central width as the separation between the two first minima. Its angular width and its width on a perpendicular screen are
The angular approximation uses radians and requires ; the screen approximation uses . The tangent relation is exact straight-line geometry, even though the underlying Fraunhofer diffraction field is approximate. This width is distinct from the full width at half maximum.
For , and , the positive first minimum is
The dimensionless far-field parameter is . Doubling the slit width to gives and parameter ; both curves below use the Fraunhofer diffraction approximation. Choosing halves those parameters and doubles both screen widths.
Figure 1.
Normalized single-slit diffraction on a screen: a narrower slit produces a wider central maximum
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Each curve is normalized to its own ; the arrows measure between first minima. The calculation uses before evaluating the sinc function, rather than replacing by . The lower diagram shows the exact screen geometry with the vertical scale enlarged. Normalization removes the change in peak brightness when the slit width changes.
The wave interference explanation is especially simple: divide the slit into equal narrow strips and add their complex amplitudes, rather than their wave intensities. With wavenumber , the continuous slit gives
Integrating the complex exponential gives the endpoint difference; its continuous value at zero is one. Taking the squared complex modulus gives the stated wave intensity. This is the Fourier transform of an interval indicator expressed in angular coordinates. Feynman's continuous-source argument obtains the same pattern by letting the number of sources tend to infinity. [ref].
At the positive first minimum, the wave phases span exactly across the slit. Every strip in one half has a partner away, with equal wave amplitude and phase difference , so the pairs cancel. At , all the wave phases align instead. [ref].
Figure 2.
Complex amplitudes across a slit: aligned contributions at broadside and cancellation at the first minimum
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The drawing uses equally weighted midpoint samples , with . At the first minimum their complex amplitudes are a common rotation of the eight roots of unity, so their head-to-tail polygon closes exactly. This finite sum illustrates cancellation; the continuous integral, rather than eight point sources, defines the slit pattern at general angles. The circle shows the continuous range of wave phases; coloured arrows show the eight samples.
A narrower aperture requires a larger angle to accumulate the cancelling phase difference, so narrowing the slit widens the beam. This is a useful limit on geometrical optics: confining light more tightly at an opening increases its subsequent angular spread. At fixed incident irradiance and slit height, reducing also reduces transmitted power, exposing a practical balance between diffraction-limited resolution and light throughput. In a diffraction grating, this single-slit diffraction envelope modulates the wave interference between different slits.
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.
Uncentered wave-field correlation Created 2026-10-14 Updated 2026-10-18
For a complex random wave amplitude, this two-point expectation retains the coherent field and uses a complex conjugate on the second amplitude. It is not a normalized wave-field correlation coefficient. Subtracting gives the centered covariance function. At coincident points the uncentered wave-field correlation equals the mean wave intensity. Under second-order stationarity it depends only on the separation and has a spectral measure of a stationary random field. A deterministic field is included by taking a degenerate ensemble.
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.
Wavefront Created 2026-10-05 Updated 2026-10-14
A wavefront connects points with the same wave phase at one specified time. It is a surface, rather than the trajectory of a particular piece of light. For a scalar monochromatic wave written as , a wavefront is a connected level set of the phase function ; different surfaces can share the same wave phase modulo . A plane wave has planar wavefronts. An outward wave from an ideal point source in a uniform medium has spheres as wavefronts, while an optical lens can turn nearly planar wavefronts into converging ones. The wavefront describes wave phase, not wave amplitude: drawing it does not say how bright the beam is. [ref]
The relation to light rays becomes precise in a stationary medium with isotropy, negligible loss and a real positive scalar refractive index . In the geometrical optics limit, spatial changes in the refractive index and wave amplitude are slow on the local wavelength scale. For a single smooth propagation branch, write
Here is the angular frequency, is the vacuum speed of light, has units of length, and the last relation is the optical eikonal equation. The local wavevector is . Its direction is normal to a smooth wavefront, since a gradient is normal to its level sets. A forward light ray has unit tangent vector , so it follows this normal under the stated assumptions. Along that light ray, : the change in is the optical path length. This is the short geometric argument linking wavefronts, light rays and optical path length. [ref]
Figure 1.
Wavefronts and normal light rays at an interface: an original plane wave model of refraction
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The diagram shows incident and transmitted branches separately, with the reflected branch omitted. Its stipulated refractive indices are and , and its incident angle is to the interface normal. At a stationary interface, the frequency and tangential wavevector agree on the two sides: Snell's law gives , hence . The wavefronts turn while their normal spacing decreases from to , where is the vacuum wavelength. More explicitly, with normal to the interface and tangential, take for and for . These functions agree at ; the drawn wavefronts are at with . This is an exact piecewise plane wave phase construction for the stipulated transparent media, not measured material data. [ref]
The normal-to-wavefront rule requires its assumptions. In a medium with anisotropy, the wavevector remains normal to a smooth wavefront, but the group velocity and energy flux need not follow it. [ref] Near a wave caustic, where multiple light rays meet, one smooth phase function may no longer describe the field; diffraction and the full wave amplitude matter. A wavefront is also not generally a surface of equal pulse arrival time. In a medium with optical dispersion, a monochromatic wave phase moves with the phase velocity, while a sufficiently narrow wave packet follows the group velocity. Even identical optical path lengths at one frequency can give different group delays. The usual equal-travel-time picture needs a common launch reference and a nondispersive ray model; an arbitrary broadband disturbance has no single monochromatic wavefront.[ref]
Waveguide cutoff frequency Created 2026-10-14 Updated 2026-10-18
The waveguide cutoff frequency separates oscillatory axial propagation from exponential decay for a particular normal mode. For the vacuum-filled rectangular electromagnetic waveguide, the dispersion relation is
For a transverse electric mode of a rectangular waveguide, are nonnegative integers but not both zero. For a mode with and nonzero , both indices must be positive. The lowest cutoff for is consequently , or ordinary frequency .
A square cross-section instead gives equal and cutoffs. The absence of a transverse electromagnetic mode is specific to this hollow pipe, rather than all electromagnetic waveguides.[ref]
For , choose real for propagation toward . For , a field decaying into a semi-infinite guide has
A finite section can contain both growing and decaying axial solutions set by its two ends; the single decaying solution is not a complete finite-section transmission calculation. At exact cutoff , the two axial solutions become a constant and a linear function of : there is no finite axial wavelength for a traveling sinusoid.
In the chosen guide at , the branch has . Its amplitude decay length is ; after , its normalized wave amplitude is . This is geometric evanescence even with ideal walls, not Joule heating. A single decaying branch has zero cycle-averaged axial Poynting vector: substituting makes a quarter-cycle out of phase with . Coupling across a finite section requires the complete boundary-value solution.
Figure 1.
Original TE10 model: propagating dispersion above cutoff and spatial amplitude decay below cutoff
. The left panel uses and to plot . The secant slope is phase velocity divided by ; the tangent slope is group velocity divided by . The right panel is the single decaying branch at , not an experimental transmission curve or a curve for dissipated power. Details.
Waveplate 2026-10-14
A waveplate uses birefringence to change polarization of an electromagnetic wave through phase retardation. Its fast axis has the smaller refractive index, hence the larger phase velocity; its slow axis has the larger index. Consider normal incidence with the optic axis in the plate face, so both components follow the same straight path. A linear polarization at to these axes excites equal wave amplitudes.
A complementary experiment uses two sheet polarizers with a cellophane sheet between them. First cross the polarizers and remove the sheet: the field is dark. Insert and rotate the sheet about the beam: light returns at intermediate orientations, but extinction recurs at two perpendicular orientations. The sheet has changed the polarization of an electromagnetic wave, without requiring a resolved double image. With white light, different wavelengths can produce different transmitted colors.[ref]. Brightness alone does not establish circular polarization: an ideal rotating linear polarizer also gives orientation-independent light intensity for unpolarized light.
At zero frequency the graded-layer transfer equation integrates to , where . Eliminating the outgoing wave amplitude at the left endpoint gives the displayed incoming-to-outgoing scattering matrix. It is real orthogonal, so it preserves total incoming and outgoing flux. It coincides with continuity of velocity and traction at a sharp seismic impedance interface; the profile between the endpoints enters at nonzero frequency.