The dislocations are not wide, the imaging condition is (weak beam fixes both).
In a strong two-beam image a dislocation is a broad, blurred dark line 10 to 15 nm wide. Tilt the crystal so your reflection is weakly excited (the g–3g condition), and the same dislocation becomes a sharp bright line about 1.5 nm wide on a nearly black background. This guide is built around the questions people ask about how and why that works, with live simulations. Example material throughout: Cu, 220 reflection, 100 kV (the case the method was invented on).
Diffraction contrast has a natural length scale: the extinction distance ξg, the depth over which intensity passes back and forth between the direct and diffracted beams. At the exact Bragg condition that exchange is slow (ξ220 ≈ 44 nm in Cu at 100 kV), and a dislocation perturbs the image over about ξg/3, 10 to 15 nm. Tilt away from Bragg and the exchange speeds up: the effective extinction distance shrinks as ξeff = ξg/√(1+(s·ξg)²). A shorter depth period gives a sharper image. Drag s and watch.
"g–3g" is a tilt recipe, read as: form the image with beam g, while tilting so that 3g sits exactly on the Bragg condition. That parks g far off Bragg (large sg), weakly excited, hence "weak beam", but in a reproducible, quotable way. Walk the steps below; the Ewald sphere, the systematic row, and the Kikuchi lines all move together.
This panel integrates the Howie–Whelan equations, the real dynamical two-beam theory, column by column through a foil containing one screw dislocation (line running into the screen). Far from the core the crystal is far off Bragg and stays dark; right beside the core the planes are locally bent back into the Bragg condition, and that narrow column lights up. That is the whole idea of weak beam. Move s and watch the broad strong-beam image narrow to a sharp line, and notice the bright line sits slightly beside the true core.
A dislocation only distorts planes that its displacement field actually bends: if the imaging reflection g is perpendicular to the Burgers vector b (so g·b = 0), those planes stay flat and the dislocation disappears. Flip through reflections and identify each segment's b: exactly the two-tilt experiment you'd run at the microscope. (For edge dislocations a weak residual image survives unless g·(b×u) is also small.)
In fcc Cu every perfect dislocation splits into two Shockley partials (b = ⅙⟨112⟩) with a ribbon of stacking fault between them. Their separation d is set by a balance: elastic repulsion pushes them apart, the fault energy γ pulls them together, so measuring d measures γ. The difficulty is that in Cu, d is only a few nm. A strong-beam image (width 10 to 15 nm) shows one blurred line; weak beam (width ~1.5 nm) resolves the pair. This is precisely the experiment Cockayne, Ray & Whelan invented the technique for in 1969.
Weak beam is dim by design: you deliberately threw away almost all the diffracted intensity to buy sharpness. Everything practical about the technique follows from that trade.
@misc{tripathy2026weakbeamdarkfield,
author = {Tripathy, Manisha},
title = {Weak-Beam Dark Field: Seeing Dislocations Sharp},
year = {2026},
howpublished = {\url{https://untetheredatom.com/tem/weak-beam-dark-field-guide}},
note = {Interactive teaching resource}
}