Contrast is not a vibe, it is a mechanism (usually three of them at once).
A TEM image is not a photograph. Nothing in the microscope "shades" the picture the way light shades the world. In conventional TEM, nearly every dark patch traces back to one of three workhorse mechanisms, often more than one at once, and reading an image correctly starts with knowing which one you're looking at.
Thicker or heavier regions scatter more electrons out of the beam → they appear darker. The "intuitive" contrast.
Crystals aligned to a Bragg condition redirect electrons into diffracted beams → they go dark in bright-field. Orientation-dependent.
Electron waves interfere. At high magnification, contrast comes from phase shifts, and flips with focus. The subtle one.
Electrons passing through more material, or heavier atoms, get scattered to higher angles and stopped by the objective aperture. Fewer electrons reach the screen, so the region looks dark. It behaves like an X-ray in reverse and mostly "means what it says." It dominates for amorphous and biological samples.
In a crystalline sample the story changes completely. A grain that happens to satisfy a Bragg condition diverts a big share of the beam into a diffracted spot. In bright-field (aperture around the direct beam) that grain goes dark: not because it's thicker or heavier, but purely because of its orientation. Tilt the sample a fraction of a degree and the darkness jumps to a different grain.
This is also where bend contours and thickness fringes come from: in a bent or wedge-shaped foil, the Bragg condition is met only along certain bands, which appear as sweeping dark curves. They move when you tilt: a dead giveaway that you're seeing diffraction contrast, not a real feature.
Zoom in far enough (high-resolution TEM), and the picture is formed by interference between the direct beam and diffracted beams. The lattice "fringes" you see are an interference pattern, and their contrast depends on defocus. Change focus slightly and atomic columns can flip from dark to bright, or vanish entirely. An HRTEM image is a fingerprint of the lattice, not a portrait of it.
A practical field guide: if the feature persists when you tilt and scales with how thick or heavy the region is, it's mass–thickness. If it moves, blinks, or sweeps when you tilt (grains flickering, contours crawling), it's diffraction contrast. If it's fine periodic fringes at high magnification that change character when you touch focus, it's phase contrast. When in doubt at the microscope: wobble the tilt and wobble the focus, and see what responds.
Mass–thickness: a simplified attenuation model. Intensity follows roughly I = I₀e^(−t/Λ), where the mean free path Λ shrinks with atomic number (elastic scattering cross-section rises steeply with Z), hence darker for thick or heavy. Treat it as a first-order trend for amorphous or weakly diffracting material, not an image-formation law for crystalline foils.
Diffraction: in a two-beam condition the direct and diffracted intensities trade off as I_g = sin²(πt s_eff)/(ξ_g s_eff)²-type expressions, with extinction distance ξ_g and excitation error s. Thickness fringes are the sin² oscillation in t; bend contours are the locus of s ≈ 0 in a curved foil.
Phase: the lens transfers each spatial frequency g with a contrast transfer function CTF(g) = sinχ(g), χ(g) = πλΔf g² + ½πC_sλ³g⁴. (Defocus sign conventions differ between texts and software; this site takes underfocus as negative Δf.) When sinχ crosses zero, that spacing disappears from the image; when it changes sign, contrast reverses. The demo above literally multiplies the lattice by sinχ.
@misc{tripathy2026thethreecontrastsoftem,
author = {Tripathy, Manisha},
title = {The Three Contrasts of TEM},
year = {2026},
howpublished = {\url{https://untetheredatom.com/tem/tem-contrast-guide}},
note = {Interactive teaching resource}
}