In mathematics, spherical harmonics are an orthogonal and complete set of functions of the spherical polar angles θ and φ. The name "spherical harmonics" is due to Lord Kelvin. In quantum mechanics they appear as eigenfunctions of orbital angular momentum. Spherical harmonics are ubiquitous in atomic and molecular physics. They are important in the representation of the gravitational field, geoid, and magnetic field of planetary bodies, characterization of the cosmic microwave background radiation and recognition of 3D shapes in computer graphics.
Definition
The notation will be reserved for functions normalized to unity. It is convenient to introduce first non-normalized functions that are proportional to the . Several definitions are possible, we start with one that is common in quantum mechanically oriented texts. The spherical polar angles are the colatitude angle θ and the longitudinal (azimuthal) angle φ. The numbers l and m are integral numbers and l is positive or zero.
where is a (phaseless) associated Legendre function.
The m dependent phase is known as the Condon & Shortley phase:
An alternative definition uses the fact that the associated Legendre functions can be defined (via the Rodrigues formula) for negative m,
The two definitions obviously agree for positive and zero m, but for negative m this is less apparent. It is also not immediately clear that the choices of phases yield the same function. However, below we will see that the definitions agree for negative m as well. Hence, for all l ≥ 0,
Complex conjugation
Noting that that the associated Legendre function is real and that
we find for the complex conjugate of the spherical harmonic in the first definition
Complex conjugation gives for the functions of positive m in the second definition
Use of the following non-trivial relation (that does not depend on any choice of phase):
gives
Since the two definitions of spherical harmonics coincide for positive m and complex conjugation gives in both definitions the same relation to functions of negative m, it follows that the two definitions agree. From here on we drop the tilde and assume both definitions to be simultaneously valid.
Note
If the m-dependent phase would be dropped in both definitions, the functions would still agree for non-negative m. However, the first definition would satisfy
whereas the second would still satisfy
from which follows that the functions would differ in phase for negative m.
Normalization
It can be shown that
The integral over φ gives 2π and a Kronecker delta on and . Thus, for the integral over θ it suffices to consider the case m = m'. The necessary integral is given here. The (non-unit) normalization of is known as Racah's normalization or Schmidt's semi-normalization. It is often more convenient than unit normalization. Unit normalized functions are defined as follows
Condon-Shortley phase
One source of confusion with the definition of the spherical harmonic functions concerns the phase factor. In quantum mechanics the phase, introduced above, is commonly used. It was introduced by Condon and Shortley.[1] In the quantum mechanics community, it is common practice to either include this phase factor in the definition of the associated Legendre functions, or to prefix it to the definition of the spherical harmonic functions, as done above. There is no requirement to use the Condon-Shortley phase in the definition of the spherical harmonic functions, but including it can simplify some quantum mechanical operations, especially the application of raising and lowering operators. The geodesy and magnetics communities never include the Condon-Shortley phase factor in their definitions of the spherical harmonic functions.
Properties
Recalling that for m ≠ 0 the associated Legendre function contains the factor (1-x²) and that the ordinary Legendre polynomial Pn(1) = 1, it follows that
The regular solid harmonics r lY lm are homogeneous of degree l in the components x, y, and z of r, so that inversion r → -r gives the factor (-1)l for the regular solid harmonics. Inversion in spherical polar coordinates is given by r → r,
θ → π-θ, and φ → π+φ. Hence
Also reflection in the x-y plane gives a phase:
Eigenfunctions of orbital angular momentum
In quantum mechanics the following operator, the orbital angular momentum operator, appears frequently
where the cross stands for the cross product of the position vector r and the gradient ∇; is Planck's constant divided by 2π.
The components of L satisfy the angular momentum commutation relations.
where εijk is the Levi-Civita symbol. In angular momentum theory it is shown that these commutation relations are sufficient to prove that L² has eigenvalues l(l+1),
where is a natural number.
From here on we take equal to unity (this is part of the system of atomic units).
The operator L² expressed in spherical polar coordinates is,
The eigenvalue equation can be simplified by separation of variables. We substitute
into the eigenvalue equation. After dividing out Ψ and multiplying with sin²θ we get
In the spirit of the method of separation of variables, we put the terms in square brackets equal
to plus and minus the same constant, respectively. Without loss of generality we take m² as this constant (m can be complex) and consider
This has the solutions
The requirement that exp[i m (φ + 2π)] = exp[i m φ] gives that m is integral. Substitution of this result into the eigenvalue equation gives
Upon writing x = cos θ the equation becomes the associated Legendre equation
This equation has two classes of solutions: the associated Legendre functions of the first and second kind. The functions of the second kind are non-regular for x = ±1 and do not concern us further. The functions of the first kind are the associated Legendre functions:
It follows that
The eigenvalue equation does not establish phase and normalization, so that these must be imposed separately. This was done earlier in this article.
Finally, noting that
we summarize two important relations holding for spherical harmonics:
Laplace equation
The Laplace equation ∇² Ψ = 0 reads in spherical polar coordinates
Clearly, this can be rewritten as
Making the Ansatz Ψ = R(r) Yml the equation can be solved readily. The solutions are known as solid harmonics. See solid harmonics for more details.
Connection with 3D full rotation group
The group of proper (no reflections) rotations in three dimensions is SO(3). It consists of all 3 x 3 orthogonal matrices with unit determinant.
A unit vector is uniquely determined by two spherical polar angles and conversely. Hence we write
Let R be a unimodular (unit determinant) orthogonal matrix, then we define a rotation operator by
The inverse matrix appears here (acting on a column vector) in order to assure that this map of rotation matrices to rotation operators is a homomorphism. Since this point was discussed at some length in Wigner's famous book on group theory, it is known as Wigner's convention. Some authors omit the inverse and find accordingly that the multiplication order of operators and matrices is reverse.
It can be shown that the rotation operator is an exponential operator in the components of the orbital angular momentum operator L. It can also be shown that the action of these operators on the spherical harmonics do no change l. That is, the linear space spanned by 2l+1 spherical harmonics of same l and different m is invariant under L, and therefore also under rotations,
The square 2l+1 dimensional matrix that appears here is known as Wigner's D-matrix. Obviously, the set of matrices of fixed l form a representation of the group SO(3). It can be shown that they form an irreducible representation of this group. The rotation operator is unitary and the spherical harmonics are orthonormal, hence the Wigner rotation matrix is a unitary matrix:
where El is the 2l+1 dimensional identity matrix.
From this unitarity follows the following useful invariance
Spherical harmonic addition theorem
The spherical harmonic addition theorem reads
There are two proofs: a short one, referred to by Whittaker and Watson[2] (p. 395) as a "physical proof", and a long analytic proof.[3]
References
- ↑ E. U. Condon and G. H. Shortley,The Theory of Atomic Spectra, Cambridge University Press, Cambridge UK (1935).
- ↑ E. T. Whittaker and G. N. Watson, A Course of Modern Analysis, Cambridge UP, Cambridge UK, 4th edition (1927)
- ↑ H. Margenau and G. M. Murphy, The Mathematics of Physics and Chemistry, 2nd edition, Van Nostrand, New York (1956), pp. 109-113. This proof involves a contour integral and several ordinary integrals
(To be continued: , real spherical harmonics, explicit expressions)