Diamond Colour Simulator

Colour Is a Defect

A perfect diamond lattice is colourless. Every colour is something that went wrong: the wrong atom, a missing one, a shear through the crystal, a stray neutron. Set what the mantle did and read the grade.

What Went Into the Lattice

Nitrogen 0 ppm

The commonest impurity. Colour depends on how it is arranged, which the mantle decides below.

Boron 0 ppm

Each single nitrogen atom cancels one boron atom, so blue needs boron in excess of single nitrogen. A few ppm of Ib nitrogen kills any natural boron content.

Hydrogen 0

Relative scale. Violet, grey and the chameleon effect all involve it.

Nickel 0

Relative scale. Green-yellow; routine in HPHT synthetics, rare in nature.

480 nm band 0

A broad absorption nobody has pinned to a defect; orange and chameleon stones carry it.

How Long the Mantle Cooked It

Temperature 1150 °C

Hotter and longer moves single nitrogen into pairs (A), then into fours (B); the N3 centres that make Cape yellow appear alongside B.

Residence 1000 Myr

Most gem diamonds sat for one to three billion years. Type Ib survives only short or cool residence. Press play to watch the nitrogen aggregate.

Late Ib growth sector 0 %

Share of the crystal that grew late and kept its nitrogen single. Real Ia/Ib stones are zoned by sector, so this renders as a second tone.

Strain

Plastic deformation 0

Shear in the mantle drags glide planes through the crystal. Also lowers clarity: graining.

Product 50
brown (vacancy clusters)pink (550 nm band)

Why some deformed stones go pink and others brown is still contested. Slide it and see.

Radiation

Dose 0

From uranium or thorium in the host rock, over millions of years. Creates GR1 vacancies: green.

Source

Alpha particles stop within about 20 microns. They leave green spots on the surface and never reach the body colour.

Heated after damage 0

Nothing to heat: there is no radiation damage yet.

Inclusions

Opaque inclusions 0

Graphite and sulphide clouds. Grey through to black.

Sub-microscopic clouds 0

These scatter light. Milky, opalescent white.

The Stone Itself

Size 1 ct

Longer light path, more absorption. A faint tint at half a carat can grade a full step deeper at five.

Nothing to anneal: no brown and no radiation damage.

The colour comes from a spectral model. Each centre contributes an absorption band; the bands sum; the transmitted light is converted to a colour the way a spectrophotometer would do it. The band shapes are illustrative, chosen so that each centre alone reproduces its documented hue, and the nitrogen aggregation kinetics are qualitative. Grade thresholds approximate GIA practice. The pink-versus-brown partition is a slider because the literature has not settled it.