In physics, and especially scattering theory, the momentum-transfer cross section (sometimes known as the momentum-transport cross section[1]) is an effective scattering cross section useful for describing the average momentum transferred from a particle when it collides with a target.
Essentially, it contains all the information about a scattering process necessary for calculating average momentum transfers but ignores other details about the scattering angle.
The momentum-transfer cross section
is defined in terms of an (azimuthally symmetric and momentum independent) differential cross section
The momentum-transfer cross section can be written in terms of the phase shifts from a partial wave analysis as [2]
Let the incoming particle be traveling along the
-axis with vector momentum
Suppose the particle scatters off the target with polar angle
and azimuthal angle
cos θ
sin θ cos ϕ
For collision to much heavier target than striking particle (ex: electron incident on the atom or ion),
≃ q cos θ
+ q sin θ cos ϕ
By conservation of momentum, the target has acquired momentum
= q ( 1 − cos θ )
− q sin θ cos ϕ
Now, if many particles scatter off the target, and the target is assumed to have azimuthal symmetry, then the radial (
) components of the transferred momentum will average to zero.
The average momentum transfer will be just
If we do the full averaging over all possible scattering events, we get
( θ , ϕ )
− q sin θ cos ϕ
where the total cross section is
Here, the averaging is done by using expected value calculation (see
as a probability density function).
Therefore, for a given total cross section, one does not need to compute new integrals for every possible momentum in order to determine the average momentum transferred to a target.
This concept is used in calculating charge radius of nuclei such as proton and deuteron by electron scattering experiments.
To this purpose a useful quantity called the scattering vector q having the dimension of inverse length is defined as a function of energy E and scattering angle θ:
sin ( θ