Sampling at makes a frequency indistinguishable from , since the extra phase is . For a real sinusoid, reflection to also gives an alias, up to phase. For example, a cosine sampled at has exactly the samples of a cosine. A measured low-frequency feature can therefore originate above the instrument's Nyquist frequency.
To reconstruct an arbitrary baseband signal limited to bandwidth , sample strictly above and use an analogue anti-aliasing filter before the sampler. A practical filter needs a transition band, so merely choosing a nominal rate is insufficient. frequency components already folded together cannot in general be separated by later digital filtering. aliasing from insufficient sampling is distinct from spectral leakage caused by a finite observation window.

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