Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
Numerical Methods in Quantum Mechanics - Dipartimento di Fisica
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Chapter 3<br />
Scatter<strong>in</strong>g from a potential<br />
Until now we have considered the <strong>di</strong>screte energy levels of simple, one-electron<br />
Hamiltonians, correspond<strong>in</strong>g to bound, localized states. Unbound, delocalized<br />
states exist as well for any physical potential (with the exception of idealized<br />
models like the harmonic potential) at sufficiently high energies. These states<br />
are relevant <strong>in</strong> the description of elastic scatter<strong>in</strong>g from a potential, i.e. processes<br />
of <strong>di</strong>ffusion of an <strong>in</strong>com<strong>in</strong>g particle. Scatter<strong>in</strong>g is a really important<br />
subject <strong>in</strong> physics, s<strong>in</strong>ce what many experiments measure is how a particle is<br />
deflected by another. The comparison of measurements with calculated results<br />
makes it possible to understand the form of the <strong>in</strong>teraction potential between<br />
the particles. In the follow<strong>in</strong>g a very short rem<strong>in</strong>der of scatter<strong>in</strong>g theory is<br />
provided; then an application to a real problem (scatter<strong>in</strong>g of H atoms by rare<br />
gas atoms) is presented. This chapter is <strong>in</strong>spired to Ch.2 (pp.14-29) of the book<br />
of Thijssen.<br />
3.1 Short rem<strong>in</strong>der of the theory of scatter<strong>in</strong>g<br />
The elastic scatter<strong>in</strong>g of a particle by another is first mapped onto the equivalent<br />
problem of elastic scatter<strong>in</strong>g from a fixed center, us<strong>in</strong>g the same coord<strong>in</strong>ate<br />
change as described <strong>in</strong> the Appen<strong>di</strong>x. In the typical geometry, a free particle,<br />
described as a plane wave with wave vector along the z axis, is <strong>in</strong>cident on the<br />
center and is scattered as a spherical wave at large values of r (<strong>di</strong>stance from the<br />
center). A typical measured quantity is the <strong>di</strong>fferential cross section dσ(Ω)/dΩ,<br />
i.e. the probability that <strong>in</strong> the unit of time a particle crosses the surface <strong>in</strong> the<br />
surface element dS = r 2 dΩ (where Ω is the solid angle, dΩ = s<strong>in</strong> θdθdφ, where<br />
θ is the polar angle and φ the azimuthal angle). Another useful quantity is the<br />
total cross section σ tot = ∫ (dσ(Ω)/dΩ)dΩ. For a central potential, the system<br />
is symmetric around the z axis and thus the <strong>di</strong>fferential cross section does not<br />
depend upon φ. The cross section depends upon the energy of the <strong>in</strong>cident<br />
particle.<br />
Let us consider a solution hav<strong>in</strong>g the form:<br />
ψ(r) = e ik·r + f(θ)<br />
r eikr (3.1)<br />
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