Fire and Dispersion

Fire in faceted gemstones – dispersion as differential refraction by wavelength, the B–G interval, named dispersion values, relationship to facet design, and distinction from diffraction-based spectral effects.

By gemmology.dev editors Last updated
phenomena/fire phenomena/dispersion refraction diamond-simulants facet-design

Definition

Fire is the splitting of white light into its spectral colours (red, orange, yellow, green,
blue, violet) visible as coloured flashes in a faceted gemstone. It arises from dispersion –
the variation of refractive index with wavelength – and is enhanced by facet geometry and
viewing conditions.

Fire is not the same as play-of-colour (opal) or labradorescence: those spectral effects
arise from diffraction or thin-film interference. Fire results from differential refraction
at every facet interface.

Mechanism

The physics of dispersion and fire:

Dispersion Defined

Refractive index (RI) varies with wavelength: shorter wavelengths (violet, blue) are
refracted more strongly at any interface than longer wavelengths (red, orange). This
wavelength-dependence of RI is dispersion. When white light enters a gem, each colour
component is refracted by a slightly different angle; on exit, the colours emerge at
different positions, producing visible spectral separation – fire.

Why Dispersion is Not Diffraction

  • Diffraction involves wave bending around apertures or at periodic structures
    (silica sphere arrays in opal, nacre platelet stacks in pearl) – structural colour.
  • Dispersion involves differential refraction at an interface between two media
    of differing refractive index – a bulk optical property of the material.

Both produce spectral colours but at entirely different physical length scales and by
different mechanisms. In a faceted gem, fire is produced at each facet face; in opal,
colour arises from the photonic crystal structure of ~200 nm silica spheres.

The B–G Interval

Gemmological dispersion is conventionally measured as the difference in refractive
index between Fraunhofer lines B (686.7 nm, deep red) and G (430.8 nm, violet):

Dispersion = n_G − n_B

A larger B–G value means greater potential for fire. Values are material constants,
independent of cut geometry.

Named Dispersion Values

B–G dispersion values for selected gem species and simulants. Source: Read (2008) [APPROXIMATE] – no single DOI-verified comprehensive dispersion table was located; diamond, zircon, and moissanite values confirmed across multiple textbook sources. CZ = 0.060 (Read 7th ed. preferred value); do NOT use 0.065 from uncited trade sources.
Species B–G Dispersion Notes
Strontium titanate (simulant) 0.190 Extremely high; immediately obvious excessive fire
Rutile (TiO₂, historical simulant) 0.280 Far exceeds diamond; strong birefringence also diagnostic
Synthetic moissanite 0.104 More than twice diamond; combined with birefringence is diagnostic
Cubic zirconia (CZ) 0.060 Higher than diamond; conspicuous fire. Note: 0.060 is the Read 7th-edition canonical value; the value 0.065 appears in some trade sources without primary citation and is not used here
GGG (gadolinium gallium garnet) 0.045 Higher than diamond; obsolete simulant
Diamond 0.044 High for natural gems; the benchmark reference value
Demantoid (andradite garnet) 0.057 Higher than diamond; contributes to demantoid's famous fire
Sphene (titanite) 0.051 Very high; softness limits durability for jewellery
YAG (yttrium aluminium garnet) 0.028 Moderate; obsolete simulant
Almandine garnet 0.027 Moderate; low fire contributes to darker appearance
Zircon (high type) 0.039 Moderate fire; good dispersion for affordable stone; also birefringent
Sapphire (corundum) 0.018 Low; fire not a notable feature of sapphire
Topaz 0.014 Low; relatively little fire
Quartz 0.013 Low
Fluorite 0.007 Very low; glass-like appearance

Facet Design and Fire

Fire is not purely a material property – cut geometry strongly determines how much
dispersion is visible:

Cut Geometry

A brilliant cut allows white light to enter through the table, undergo total internal
reflection at the pavilion facets, and exit through the crown facets. Each reflection
and refraction event disperses the light further. The crown height, facet angles, and
number of facets all influence how the dispersed colours emerge to the viewer.

Very shallow or very deep pavilion angles reduce total internal reflection and therefore
reduce both brilliance and fire.

Trade-off with Brilliance

High dispersion often correlates with high RI (both increase as electron density
increases). However, brilliance (white light return) and fire compete in cut design:

  • A broad table suppresses fire (less crown facet area to produce coloured flashes)
  • More and smaller crown facets generate more fire at the cost of some brilliance
  • The classic round brilliant optimises both for diamond

Distinguishing Fire from Other Spectral Effects

Fire versus diffraction-based and interference-based spectral colour effects
Effect Mechanism Visual Character Host Material
Fire (dispersion) Differential refraction at gem facets Coloured flashes that change with viewing angle; seen in faceted gems Faceted stones
Play-of-colour (opal) Diffraction from silica sphere array (~200 nm) Spectral colour patches shifting with viewing angle; cabochon or rough Precious opal
Labradorescence Thin-film interference in Bøggild intergrowth Directional broad colour zones in feldspar; not rapid flashes Labradorite feldspar
Orient (pearl) Thin-film diffraction/interference in nacre platelets Soft iridescent surface bloom; not rapid flashes Nacre-covered pearls
Iridescence (general) Thin-film interference or diffraction Broad spectral sheen associated with surface or near-surface structure Fire agate, ammolite, surface films

Diagnostic Relevance

Using dispersion in gem identification:

High Fire as Diagnostic

Fire conspicuously greater than diamond narrows identification to a short list.
Combine dispersion observation with RI, SG, and optic character:

  • Excessive fire + birefringence (doubling of facet edges) = moissanite
  • Excessive fire + high SG, no birefringence = CZ or GGG (historical)
  • Extreme fire + very high birefringence = rutile or synthetic rutile (historical)

Low Fire as Diagnostic

A colourless stone with very little fire but high RI may be zircon (also birefringent
under magnification) or a heavy-element glass. Sapphire has low dispersion (0.018) so
shows little fire despite its relatively high RI.

Sources

Read (2008)

Gemmology (3rd ed.). Butterworth-Heinemann/Routledge. DOI: 10.4324/9780080507224. [APPROXIMATE – chapter confirmed; page references not independently verified] – Primary source for dispersion mechanism and B–G values. No single DOI-verified comprehensive dispersion table paper was located in the source research session; values are textbook-consensus and should be verified against a primary spectrophotometric source before formal examination use. [Confidence C for the full dispersion table]

Nassau (2001)

The Physics and Chemistry of Color (2nd ed.). Wiley-Interscience. No DOI retrieved. [UNVERIFIED] – Conceptual support for dispersion mechanism.