Moiré fringes arise when two overlapping periodic structures contribute closely spaced reciprocal lattice vectors to the transmission electron microscopy image. Their relative phase varies slowly across the image, producing a coarse modulation with a period much larger than either atomic spacing. The structures may have different lattice spacings, a small relative rotation, or both. The modulation is an interference or beat phenomenon; its spacing is not itself a new atomic-plane spacing. Its orientation is perpendicular to the difference vector of the two contributing projected reciprocal-lattice vectors.
Let the relevant projected reciprocal lattice vectors have magnitudes and , with angle between them. Subtracting their phases gives the slow spatial modulation . The moiré fringe spacing formula is thereforeFor parallel planes, and . For equal spacings, at a small angle measured in radians. The apparent divergence as both mismatch and rotation vanish means that there is no finite beat period; it does not predict an infinite number of visible fringes.
For each spacing pair, the largest geometrical period occurs with parallel projected reciprocal vectors. The closest pair is and , givingHowever, the crystal is only across. It contains at most of this period, so the largest formal period cannot appear as a repeated fringe train inside one crystal. It can instead give a broad variation of contrast. A period of order the particle diameter is the largest directly sampled scale, and even that is poorly constrained by one particle.
The distinction matters if “see” means a complete repeat. Of the exactly parallel spacing pairs, the largest other period is approximately from the and pair. If relative rotation is continuously variable, the closest pair can instead be rotated slightly to shorten its period below , so is not a universal maximum visible period for arbitrary orientations.
A coarse fringe in a high-resolution transmission electron microscopy image need not directly identify the lattice spacing of a new phase. Check whether overlapping crystals, a particle and its substrate, or differently oriented domains can produce the corresponding moiré fringe. Compare the underlying reciprocal-space peaks and their difference, use the particle boundary to constrain how many periods are actually sampled, and examine neighbouring or differently oriented regions. For the closest pair here, fitting a periodicity from less than one complete period is particularly unreliable. Distinguishing lattice contrast from a beat envelope prevents misidentifying a phase or over-interpreting local strain.
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