In plain words

How much a thin stands out from the surface it sits on under a microscope. On the right base – usually silicon coated with a thin layer of glassy oxide – even a of atoms becomes visible through an ordinary optical microscope, thanks to the same effect that paints colours on a soap bubble.

Going deeper

Left: light reflecting from the top of a flake and from the interfaces of the oxide beneath it, the two paths interfering. Right: contrast in green light against oxide thickness, oscillating with maxima near 90 nm and 285 nm and vanishing in between. why one atom thick can be seen at all silicon silicon oxide flake light reflected from the top and from below the oxide interferes: the flake changes the balance it depends on the oxide, and on the colour contrast, green light oxide thickness (nm) ≈ 90 ≈ 285 300 nm is usual; about 100 nm is better
A single layer absorbs only a few percent of light, yet it is visible under an ordinary microscope on the right substrate: light reflected from the flake interferes with light reflected from beneath the oxide, and the flake shifts the balance. Which oxide thickness works depends on the colour of the light.

Interference, not absorption

Graphene absorbs about 2.3% of visible light – far too little to see directly. What makes it visible is interference. Light reflected from the top surface of the flake and light that travels down through the oxide, reflects from the silicon and comes back, meet again with a phase difference set by the oxide thickness and the wavelength. Adding one atomic layer changes both the amplitude and the phase of the first reflection, and near the right thickness that small change alters the total reflected intensity by several percent – enough for the eye.

A Fresnel-law calculation reproduces the measured contrast quantitatively, which is why the effect can be designed rather than discovered by trial.

Choosing the substrate and the light

Because the interference condition depends on both thickness and wavelength, the standard 300 nm oxide gives good contrast for green light but poor contrast at other colours, and a flake that is obvious under one filter can vanish under another. About 100 nm of oxide is better still for visual detection, and with monochromatic illumination almost any oxide thickness can be made to work by choosing the wavelength.

The same reasoning extends beyond graphene: monolayers are found on tuned oxides in the same way, and the contrast against thickness curve is used to count layers, since each added layer changes the reflected intensity in a roughly stepwise manner. On unoptimised – sapphire, glass, thick metal – flakes can be nearly invisible, which is a real obstacle when transferring onto arbitrary targets.

A quick tool, with limits

Optical contrast is the fastest way to find flakes and to guess a layer count: it needs no vacuum, no contact and no damage, and it can be automated, which is how large flake-searching setups scan whole .

It is not a measurement of thickness, though. Contrast depends on illumination spectrum, camera response, objective numerical aperture, oxide thickness tolerance and any residue under the flake, so calibration is per setup rather than universal. The sensible practice is to calibrate against or once on a given microscope and substrate, then use contrast as the routine screen – and to treat any absolute layer assignment from contrast alone as provisional.

For specialists

The difference in reflected intensity between a flake and its substrate, enhanced by thin-film interference in the oxide layer.

Where this comes from

  1. Making graphene visible Blake et al. · Applied Physics Letters 91, 063124 (2007) cited by 1,799
  2. Fine structure constant defines visual transparency of graphene Nair et al. · Science 320, 1308 (2008) cited by 9,117
  3. Visibility of dichalcogenide nanolayers Benameur et al. · Nanotechnology 22, 125706 (2011) cited by 452