Bipolar gradient 2026-11-05
A bipolar gradient is a magnetic field gradient waveform with lobes of opposite sign. In nuclear magnetic resonance, such waveforms can control sensitivity to position and motion. Opposite signs alone do not guarantee equal signed areas, and an applied waveform must be distinguished from its effective encoding waveform when refocusing pulses change phase evolution.
For an original counterexample, apply for and then for . The gradient zeroth moment is
The waveform is bipolar but unbalanced.
If the two durations are instead equal to , and the effective lobes are contiguous, from time 0 to and from to , then but the gradient first moment is . Thus cancellation of stationary-position phase can coexist with sensitivity to constant velocity. The sign follows this stated ordering.
Bipolar pulses also appear outside flow imaging. A 1989 stimulated echo study addressed background gradients that distort diffusion measurements. Alternating pulses could cancel a cross term under specified conditions; tests used proton signals from homogeneous and granular samples.[ref] This is a sequence-specific result, not a promise that every bipolar pair removes every imaging error.
Gradient first moment 2026-11-05
The gradient first moment of an effective magnetic field gradient waveform is its time-weighted integral,
Here effective includes the sign changes caused by refocusing pulses. Its units are when is in tesla per metre. The gradient zeroth moment is . For position with constant velocity, the accumulated nuclear magnetic resonance phase is
where is the angular gyromagnetic ratio. Thus removes the dependence on initial position while can retain sensitivity to velocity, the basis of an idealized phase-contrast magnetic resonance imaging encoding.[ref]
For a teaching bipolar gradient, let the first lobe have signed area and time centroid , and the second have signed area and centroid . Then
Equal and opposite lobe areas cancel stationary-spin phase, but their time separation prevents cancellation of the constant-velocity phase. For and , the first moment is . These are illustrative waveform values, not measurements from the source.
The time origin is part of the definition: replacing by gives . Balanced makes the first moment independent of that choice. Two encodings with equal zeroth moments use their first-moment difference , rather than either individual value, to infer velocity.