A Lippmann plate records colour as a depth-dependent optical structure in a photographic emulsion. A standing wave writes a spacing; wave interference during later illumination selects the reflected wavelengths. This makes a photographic plate a spatial record of an optical spectrum. The striking idea is that information about colour can live in geometry.
Gabriel Lippmann presented his colour process in 1891 and received the 1908 Nobel Prize in Physics. His career belongs principally to physics: he held chairs in mathematical and experimental physics.[ref] [ref]
In his 14 December 1908 Nobel lecture, Gabriel Lippmann described a photographic plate bearing a transparent, even, extremely fine sensitive layer. A holder put Mercury against that layer as a mirror during exposure. Incident and reflected light formed a standing wave within the photographic emulsion; after photographic processing and drying, white light revealed colour by selective reflection. The reflector served during recording; the developed structure supplied the later colour selection.[ref]
The lecture's control was to project a spectrum photograph, wet it, and project it again. Its colours disappeared as the gelatin swelled, then returned during drying, red before the shorter wavelengths. This tested a spacing-dependent explanation. Lippmann also reported roughly one-minute sunlight exposures and identified portrait exposure time as a limitation.[ref]
A reversible colour change supports a structural explanation, but does not independently measure every fringe spacing or the refractive index. For a conceptual comparison, record a narrow band and compare reflected optical spectra at fixed illumination and viewing angles; an unexposed processed plate tests background. A second comparison changes only viewing geometry. A third compares the dry state before and after a reversible spacing change. These are proposed discriminating controls, not additional experiments attributed to Lippmann. Background surface reflection must be separated from the selective signal. A photograph's appearance also depends on the illuminating optical spectrum; viewing under an arbitrary lamp is not a calibrated spectral measurement.
At normal incidence, let measure distance from the reflector into a uniform transparent layer with refractive index . For a monochromatic wave of vacuum wavelength , the layer wavenumber is . Represent the incident and returning electric fields by complex wave amplitudes with time factor suppressed:
The time-averaged squared electric field, normalized to the incident contribution, is
This electric exposure pattern has maxima separated by
The wave phase of the reflector shifts the maxima's positions but leaves their spacing unchanged in this uniform-layer model. The electric pattern, rather than the zero net energy flux of an ideal standing wave, is the relevant exposure proxy. An imperfect mirror reduces its contrast: , where denotes this exposure proxy.
Choose and . Then the medium wavelength is and . For an ideal phase-reversing reflector, and the normalized pattern is : its first two maxima are at and . These are chosen calculations, not measured properties of a historical photographic emulsion or the optical response of Mercury.
Figure 1.
A standing wave records depth fringes apart
. Original schematic and calculation for chosen , and an ideal phase-reversing mirror. The upper diagram distinguishes recording with a reflector from later reflected-colour readout. The lower plot shows the normalized electric exposure pattern, not a measured developed density profile. The first fringe position depends on reflector wave phase; the period does not. Material widths in the apparatus schematic are illustrative. Source. Details.
For multiple mutually incoherent wavelengths, time averaging adds exposure contributions rather than their instantaneous electric fields. In a linearized recording model,
Here is incident spectral exposure density, a wavelength-dependent recording sensitivity and a model exposure response. An optical spectrum therefore writes overlapping depth oscillations, not necessarily visibly separated sheets. This is a useful connection to the Fourier transform: approximately, depth is paired with optical spatial frequency . Finite recording depth, varying sensitivity and nonlinear photographic processing prevent treating this expression as an exact inversion rule for an actual plate.
To isolate the readout mechanism, replace the processed photographic emulsion by equally spaced, identical weak scattering planes, with separation . Take the readout refractive index to be real and independent of wavelength, and let be the internal angle from the plane normal. Adjacent specularly backscattered contributions differ in wave phase by . Their geometric series gives
Here is a small plane reflection wave amplitude, assumed constant in this illustrative band; at by continuity. Since incident and reflected waves occupy the same external medium, is the model reflectance when transmission factors are absorbed into . Require for the weak-scattering sum to remain self-consistent. Normalizing to discards absolute brightness; it does not predict a highly reflecting historical plate.
The first-order peak obeys
This is Bragg's law with an angle measured from the normal, rather than the glancing Bragg angle. For external viewing angle in air approximated by refractive index one, Snell's law gives , hence
The expression describes specular readout: illumination must supply the matching incident direction. Tilting a plate under fixed narrow illumination can make the signal disappear as well as change its selected colour.
For the chosen and , calculated peaks are at , at , and at . Greater obliquity selects a shorter wavelength. Uniform shrinkage to , with unchanged , multiplies every peak wavelength by : a chosen moves the normal peak to . More generally, at normal incidence. A change of thickness alone is insufficient if processing also changes the refractive index.
Finite gives a finite spectral response. The nearest zeros satisfy , giving . At the normal peak, gives neighbouring zeros at approximately and ; gives and . Thus greater sampled depth narrows the central band in this model. The small-detuning distance from peak to a nearest zero is approximately ; it is not the full width at half maximum.
Figure 1.
Calculated angular colour shift and finite-stack reflectance shape
. Original weak-scattering finite-grating model with chosen and . Left: predicted first-order peak versus external angle, with a separate illustrative 5 percent shrinkage calculation at unchanged refractive index. Right: normalized , comparing and at normal readout and at external readout. Every curve is calculated; none is a measured spectrum. Source. Details.
Real processed photographic emulsions have a continuous, irregular depth response rather than identical planes. Absorption, wavelength-dependent refractive index, unequal scattering strengths, a nonideal exposure reflector, changes during photographic processing and multiple scattering of light can alter both peak positions and shapes. A transfer calculation with measured material parameters would be needed for quantitative reflectance. The present model explains the phase-selection mechanism and the tradeoff between depth and spectral width; it cannot establish faithful reproduction of an arbitrary incident optical spectrum. Its useful lesson is that a photograph can record colour through sub-wavelength structure, while its eventual appearance still depends on illumination, viewing geometry and processing.

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