The differential scattering cross-section is the effective incident area scattered per unit solid angle. It is defined by the ratio of the outgoing particle rate through to the incident flux.
For an azimuthally symmetric classical scattering map from impact parameter to scattering angle ,When several impact parameters produce the same angle, their nonnegative contributions are summed.
Ifthen the ratio of scattered radial probability current through to the incident probability flux is
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