Depth turns a local field into a projection
The local field is uniform through the chosen thickness. Without crystal coupling, doubling thickness doubles the expected impulse; it does not identify an unknown depth profile.
E38 · Electron imaging
When does the shift of the diffraction disk measure the field in the specimen? Only when three things hold: the zero position is calibrated on a vacuum reference, the detector covers all the relevant angles, and scattering in the specimen doesn't reshape the disk. Even then, the shift measures only the total sideways push on the beam through the specimen. An electric or a magnetic field could give the same push, so one scan can't tell them apart.
Send a converging electron probe through a smooth junction and compare its diffraction disk with a separately recorded vacuum disk. Turn the measured center-of-mass shift into an electric-equivalent projected field, compare it with the quadrant-difference estimate, and see how clipping, counting noise and crystal scattering can imitate a field.
Physics tutorial
BackgroundAn electron that crosses a region with a smooth sideways force picks up sideways momentum, and its diffraction disk shifts. If the disk shifts without changing shape, a pixelated detector can measure the shift from the centroid of the recorded intensity.
Why it mattersThe apparent field also depends on where the detector zero lies, on angles the detector misses, on counting noise and on intensity the crystal scatters elsewhere.
Start with the essentials
The local field is uniform through the chosen thickness. Without crystal coupling, doubling thickness doubles the expected impulse; it does not identify an unknown depth profile.
The coupling c and excitation error determine reversible elastic transfer. A nonzero disk centroid can therefore occur with no electromagnetic field.
The beam travels along positive z through the specimen. A positive projected electric field along x pushes the electron toward negative x, and a negative projected magnetic induction along y gives the same shift. The beam is fixed at 200 kV.
The separate vacuum frame uses the same angular mask. Every scan point shares this one reference, so its counting error appears at every point. Clipping can bias the specimen and vacuum centroids by different amounts.
Its unit is volts because it is a field integrated through the depth of the specimen, not the local field in volts per meter. The magnetic preset produces the same counts with no electric field at all.
This slope holds for a complete, uniform circular disk that moves only a little. Large offsets make the relation nonlinear, and an annular mask or a partly lost disk changes the calibration.
Each scan has 24 by 24 exposures at 2 nm spacing. The separate vacuum exposure adds acquisition time and data but no specimen dose. The error shown against the known model uses the probe-blurred projected field as its reference.
Typical misconceptionThe map gives a unique electric field at each atom.
Better mental modelThe map shows an electric-equivalent field integrated through the depth and averaged over the probe. Magnetic forces and scattering can contribute, and the Lab does no atomic multislice calculation.
Typical misconceptionA symmetric detector mask guarantees an unbiased centroid.
Better mental modelIf the shifted disk is cut differently from the vacuum disk, the symmetry of the mask does not restore the missing intensity.
With crystal coupling off, drag the specimen from 100 to 50 nm and compare the recovered projection. Then choose No field · lattice impulse and vary thickness and mistilt.
What to observe: The field contribution scales with path length. Elastic two-beam exchange varies non-monotonically and can create an apparent field even when the true field is zero.Compare the uncalibrated state with Calibrated center of mass.
What to observe: Subtracting the measured vacuum counts removes the detector offset, but the noise in the reference stays.Shrink the outer mask or exclude an inner region.
What to observe: The centroid of a clipped disk no longer gives the average momentum of the whole beam. Missing counts can make both estimates invalid.Compare the quadrant and scattering-artefact presets, then the magnetic preset.
What to observe: The quadrant estimate drifts away from its small-shift calibration, and elastic dynamical diffraction creates false field contrast. Electric and magnetic sources can produce identical shift data.Turn on vacuum correction, meet the stated limits on acceptance, counts, RMS error and dose, then check.
What to observe: More exposure lowers counting noise, but it cannot remove the systematic bias from clipping or scattering.