14.3: Partial Waves
( \newcommand{\kernel}{\mathrm{null}\,}\)
We can assume, without loss of generality, that the incident wavefunction is characterized by a wavevector k that is aligned parallel to the z-axis. The scattered wavefunction is characterized by a wavevector k′ that has the same magnitude as k, but, in general, points in a different direction. The direction of k′ is specified by the polar angle θ (i.e., the angle subtended between the two wavevectors), and an azimuthal angle ϕ about the z-axis. Equations ([e17.38]) and ([e17.39]) strongly suggest that for a spherically symmetric scattering potential [i.e., V(r)=V(r)] the scattering amplitude is a function of θ only: that is, f(θ,ϕ)=f(θ). It follows that neither the incident wavefunction,
ψ0(r)=√nexp(ikz)=√nexp(ikrcosθ), nor the large-r form of the total wavefunction,
ψ(r)=√n[exp(ikrcosθ)+exp(ikr)f(θ)r], depend on the azimuthal angle ϕ.
Outside the range of the scattering potential, both ψ0(r) and ψ(r) satisfy the free-space Schrödinger equation,
(∇2+k2)ψ=0. What is the most general solution to this equation in spherical polar coordinates that does not depend on the azimuthal angle ϕ? Separation of variables yields
ψ(r,θ)=∑lRl(r)Pl(cosθ), because the Legendre functions, Pl(cosθ), form a complete set in θ-space. The Legendre functions are related to the spherical harmonics, introduced in Chapter [sorb], via Pl(cosθ)=√4π2l+1Yl,0(θ,φ). Equations ([e17.54]) and ([e17.55]) can be combined to give
r2d2Rldr2+2rdRldr+[k2r2−l(l+1)]Rl=0. The two independent solutions to this equation are the spherical Bessel functions, jl(kr) and yl(kr), introduced in Section [rwell]. Recall that
jl(z)=zl(−1zddz)l(sinzz),yl(z)=−zl(−1zddz)l(coszz). Note that the jl(z) are well behaved in the limit z→0, whereas the yl(z) become singular. The asymptotic behavior of these functions in the limit z→∞ is
jl(z)→sin(z−lπ/2)z,yl(z)→−cos(z−lπ/2)z.
We can write exp(ikrcosθ)=∑laljl(kr)Pl(cosθ), where the al are constants. Note there are no yl(kr) functions in this expression because they are not well-behaved as r→0. The Legendre functions are orthonormal ,
∫1−1Pn(μ)Pm(μ)dμ=δnmn+1/2, so we can invert the previous expansion to give aljl(kr)=(l+1/2)∫1−1exp(ikrμ)Pl(μ)dμ. It is well known that jl(y)=(−i)l2∫1−1exp(iyμ)Pl(μ)dμ, where l=0,1,2,⋯. Thus, al=il(2l+1), giving
ψ0(r)=√nexp(ikrcosθ)=√n∑lil(2l+1)jl(kr)Pl(cosθ). The previous expression tells us how to decompose the incident plane-wave into a series of spherical waves. These waves are usually termed “partial waves”.
The most general expression for the total wavefunction outside the scattering region is ψ(r)=√n∑l[Aljl(kr)+Blyl(kr)]Pl(cosθ), where the Al and Bl are constants. Note that the yl(kr) functions are allowed to appear in this expansion because its region of validity does not include the origin. In the large-r limit, the total wavefunction reduces to ψ(r)≃√n∑l[Alsin(kr−lπ/2)kr−Blcos(kr−lπ/2)kr]Pl(cosθ), where use has been made of Equations ([e17.59a]) and ([e17.59b]). The previous expression can also be written
ψ(r)≃√n∑lClsin(kr−lπ/2+δl)krPl(cosθ), where the sine and cosine functions have been combined to give a sine function which is phase-shifted by δl. Note that Al=Clcosδl and Bl=−Clsinδl.
Equation ([e17.68]) yields ψ(r)≃√n∑lCl[ei(kr−lπ/2+δl)−e−i(kr−lπ/2+δl)2ikr]Pl(cosθ), which contains both incoming and outgoing spherical waves. What is the source of the incoming waves? Obviously, they must be part of the large-r asymptotic expansion of the incident wavefunction. In fact, it is easily seen from Equations ([e17.59a]) and ([e15.49]) that
ψ0(r)≃√n∑lil(2l+1)[ei(kr−lπ/2)−e−i(kr−lπ/2)2ikr]Pl(cosθ) in the large-r limit. Now, Equations ([e17.52]) and ([e17.53]) give
ψ(r)−ψ0(r)√n=exp(ikr)rf(θ). Note that the right-hand side consists of an outgoing spherical wave only. This implies that the coefficients of the incoming spherical waves in the large-r expansions of ψ(r) and ψ0(r) must be the same. It follows from Equations ([e17.69]) and ([e17.70]) that Cl=(2l+1)exp[i(δl+lπ/2)]. Thus, Equations ([e17.69])–([e17.71]) yield
f(θ)=∑l=0,∞(2l+1)exp(iδl)ksinδlPl(cosθ). Clearly, determining the scattering amplitude, f(θ), via a decomposition into partial waves (i.e., spherical waves) is equivalent to determining the phase-shifts, δl.
Now, the differential scattering cross-section, dσ/dΩ, is simply the modulus squared of the scattering amplitude, f(θ). [See Equation ([e15.17]).] The total cross-section is thus given by σtotal=∫|f(θ)|2dΩ=1k2∮dϕ∫1−1dμ∑l∑l′(2l+1)(2l′+1)exp[i(δl−δl′)]sinδlsinδl′Pl(μ)Pl′(μ), where μ=cosθ. It follows that σtotal=4πk2∑l(2l+1)sin2δl, where use has been made of Equation ([e17.61]).
Contributors and Attributions
Richard Fitzpatrick (Professor of Physics, The University of Texas at Austin)