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Introduction

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The acoustic scattering problem for a sphere separates exactly in spherical coordinates. The incident, scattered, and interior fields can therefore be expanded in spherical eigenfunctions, and the boundary conditions reduce to independent algebraic equations for each angular order (Anderson 1950).

The spherical modal-series solution applies that structure to fixed-rigid, pressure-release, liquid-filled, and gas-filled spheres. Medium 1 is the surrounding fluid and medium 2 is the sphere interior.

Symbols and medium indexing follow Notation and Symbols. The physical meaning of each interface type is developed in Boundary Conditions.

The unshelled problem has three boundary families. A fixed-rigid sphere enforces zero normal velocity at r=a, a pressure-release sphere enforces zero pressure, and a penetrable sphere enforces pressure and normal-velocity continuity. Elastic solids and shells require additional displacement and traction conditions and are treated by SOEMS and ESSMS.

The boundary condition is imposed at r = a, the incident and scattered fields are expanded in spherical partial waves outside the sphere, and the interior field is expanded in regular spherical waves inside the sphere. The polar angle \theta identifies the usual axisymmetric geometry, while the coefficient A_n carries the scattered contribution of angular order n.

Reduction of the wave equation in spherical coordinates

Helmholtz equation in the surrounding fluid

In a homogeneous inviscid fluid, the time-harmonic acoustic pressure satisfies:

\nabla^2 p + k^2 p = 0,

where k = \omega/c. In spherical coordinates (r,\theta,\varphi), the Laplacian becomes:

\nabla^2 p = \frac{1}{r^2}\frac{\partial}{\partial r} \left(r^2\frac{\partial p}{\partial r}\right) + \frac{1}{r^2 \sin\theta}\frac{\partial}{\partial \theta} \left(\sin\theta\frac{\partial p}{\partial \theta}\right) + \frac{1}{r^2\sin^2\theta}\frac{\partial^2 p}{\partial \varphi^2}.

For axisymmetric incidence, the field is independent of \varphi, so the last term vanishes.

Separation of variables

The axisymmetric pressure can be expressed as a product of radial and angular factors:

p(r,\theta) = R(r)\Theta(\theta),

where R(r) represents the radial dependence of the pressure field and \Theta(\theta) represents the angular dependence. Substituting this product into the Helmholtz equation and separating radial from angular dependence gives:

\frac{1}{R}\frac{d}{dr} \left(r^2\frac{dR}{dr}\right) + k^2r^2 = -\frac{1}{\Theta\sin\theta} \frac{d}{d\theta}\left(\sin\theta\frac{d\Theta}{d\theta}\right).

Because the left-hand side depends only on r and the right-hand side depends only on \theta, both sides must equal the same separation constant. Writing that constant as n(n+1) gives the angular equation:

\frac{1}{\sin\theta} \frac{d}{d\theta} \left(\sin\theta\frac{d\Theta}{d\theta}\right) + n(n+1)\Theta = 0,

whose regular solutions are the Legendre polynomials:

\Theta(\theta) = P_n(\cos\theta).

The radial equation takes the form:

\frac{d}{dr}\left(r^2\frac{dR}{dr}\right) + \left(k^2r^2 - n(n+1)\right)R = 0,

whose independent solutions are the spherical Bessel, Neumann, and Hankel functions. Spherical geometry keeps the angular order n separated, so each partial wave can be solved independently after the boundary condition is imposed (Morse and Feshbach 1953).

Orthogonality

The angular modes decouple because the Legendre polynomials satisfy:

\int_{-1}^{1} P_m(\mu)P_n(\mu)\,d\mu = \frac{2}{2n+1}\delta_{mn}.

This orthogonality turns the continuous boundary conditions into independent equations for each order n.

Incident and scattered field expansions

Incident plane wave

Let P_0 denote the incident pressure amplitude. A plane wave propagating along the polar axis is expanded as:

p_{1,\text{inc}}(r,\theta) = P_0 e^{ik_1r\cos\theta} = P_0\sum_{n=0}^{\infty}(2n+1)i^n \text{j}_n(k_1r)P_n(\cos\theta).

The use of \text{j}_n is the spherical analogue of using a regular interior radial basis in other modal solutions. Although the incident plane wave is physically defined in the exterior region, its modal expansion is written in terms of the regular spherical Bessel functions because those are the nonsingular basis functions associated with the separated radial equation.

Exterior scattered field

The exterior scattered field must satisfy the Sommerfeld radiation condition (Sommerfeld 1949) and is therefore expanded in outgoing spherical Hankel functions:

p_{1,\text{scat}}(r,\theta) = P_0\sum_{n=0}^{\infty}(2n+1)i^n A_n h_n^{(1)}(k_1r)P_n(\cos\theta).

The coefficients A_n are determined by the boundary conditions.

Far-field backscatter

Using the large-argument asymptotic form:

h_n^{(1)}(kr) \sim \frac{(-i)^{n+1}e^{ikr}}{kr}, \qquad r \to \infty,

the scattered field becomes:

p_{1,\text{scat}}(r,\theta) \sim P_0\frac{e^{ik_1r}}{r} \left[-\frac{i}{k_1} \sum_{n=0}^{\infty}(2n+1)A_nP_n(\cos\theta) \right].

In the backscattering direction \theta = \pi, one has P_n(-1) = (-1)^n, so the backscattering amplitude is:

\mathcal{f}_\text{bs} = -\frac{i}{k_1} \sum_{n=0}^{\infty}(-1)^n(2n+1)A_n.

Boundary-condition derivations

Fixed rigid sphere

For a rigid sphere of radius a, the normal fluid velocity vanishes at the surface. Since particle velocity is proportional to the normal derivative of pressure, the boundary condition is:

\left.\frac{\partial}{\partial r}(p_{1,\text{inc}}+p_{1,\text{scat}})\right|_{r=a} = 0.

Substituting the modal expansions and using orthogonality gives, for each order n:

\text{j}_n^\prime(k_1a) + A_n h_n^{(1)\,\prime}(k_1a) = 0.

This boundary condition gives the scattered partial-wave coefficient:

A_n = -\frac{\text{j}_n^\prime(k_1a)}{h_n^{(1)\,\prime}(k_1a)}.

Pressure-release sphere

For a pressure-release boundary, the total pressure vanishes at the surface:

p_{1,\text{inc}}(a,\theta) + p_{1,\text{scat}}(a,\theta) = 0.

Substitution of the modal expansions gives, mode by mode:

\text{j}_n(k_1a) + A_n h_n^{(1)}(k_1a) = 0.

This boundary condition gives the scattered partial-wave coefficient:

A_n = -\frac{\text{j}_n(k_1a)}{h_n^{(1)}(k_1a)}.

Fluid-filled and gas-filled sphere

For a fluid or gas interior, the pressure inside the sphere must remain finite at the origin, so the interior field is expanded in regular spherical Bessel functions. Writing the interior density and wavenumber as \rho_2 and k_2, the interior field becomes:

p_2(r,\theta) = P_0\sum_{n=0}^{\infty}(2n+1)i^n B_n \text{j}_n(k_2r)P_n(\cos\theta).

At r = a, pressure and normal velocity are continuous. In region-indexed notation, the pressure condition is:

p_1 = p_2,

The corresponding normal-velocity condition is:

\frac{1}{\rho_1}\frac{\partial p_1}{\partial r} = \frac{1}{\rho_2}\frac{\partial p_2}{\partial r}.

Since the exterior total pressure is p_1 = p_{1,\text{inc}} + p_{1,\text{scat}}, substituting the modal expansions gives, for each order n:

\begin{align*} \text{j}_n(k_1a) + A_n h_n^{(1)}(k_1a) &= B_n \text{j}_n(k_2a), \\ \frac{k_1}{\rho_1}\left[\text{j}_n^\prime(k_1a) + A_n h_n^{(1)\,\prime}(k_1a)\right] &= \frac{k_2}{\rho_2}B_n \text{j}_n^\prime(k_2a). \end{align*}

Solving the pressure-continuity equation for the interior coefficient gives:

B_n = \frac{\text{j}_n(k_1 a) + A_n h_n^{(1)}(k_1 a)} {\text{j}_n(k_2 a)}.

Substituting that result into the velocity condition yields:

\text{j}_n^\prime(k_1 a) + A_n h_n^{(1)\,\prime}(k_1 a) = \frac{\rho_1 k_2}{\rho_2 k_1} \frac{\text{j}_n^\prime(k_2 a)}{\text{j}_n(k_2 a)} \left[\text{j}_n(k_1 a) + A_n h_n^{(1)}(k_1 a)\right]

Now define the density and sound-speed contrasts by:

g_{21} = \frac{\rho_2}{\rho_1}, \qquad h_{21} = \frac{c_2}{c_1}

Because k_2/k_1 = 1/h_{21}, the prefactor \rho_1 k_2 / (\rho_2 k_1) becomes 1/(g_{21}h_{21}). Rearranging the continuity equations therefore gives:

A_n \left[ h_n^{(1)\,\prime}(k_1 a) -\frac{1}{g_{21}h_{21}} \frac{\text{j}_n'(k_2 a)}{\text{j}_n(k_2 a)} h_n^{(1)}(k_1 a) \right] = \\ \frac{1}{g_{21}h_{21}} \frac{\text{j}_n'(k_2 a)}{\text{j}_n(k_2 a)} \text{j}_n(k_1 a) -\text{j}_n'(k_1 a)

The scattered partial-wave coefficient can therefore be written explicitly as:

A_n = \frac{ \dfrac{1}{g_{21}h_{21}}\dfrac{\text{j}_n^\prime(k_2 a)}{\text{j}_n(k_2 a)}\text{j}_n(k_1 a) - \text{j}_n^\prime(k_1 a) }{ h_n^{(1)\,\prime}(k_1 a) - \dfrac{1}{g_{21}h_{21}}\dfrac{\text{j}_n^\prime(k_2 a)}{\text{j}_n(k_2 a)}h_n^{(1)}(k_1 a) }

The interior amplitude has now been eliminated from the 2\times2 continuity system. Liquid-filled and gas-filled spheres use the same coefficient equation (Anderson 1950). Their physical distinction lies in the values of g_{21} and h_{21}, which are usually much farther from unity for a gas.

The exact solution is an infinite partial-wave series. In practice only finitely many modes contribute appreciably at fixed acoustic size. The required number of modes increases with k_1 a because higher angular orders resolve finer angular variation along the sphere.

This is a general feature of all modal scattering solutions and follows from the fact that the angular spectrum broadens as the target becomes acoustically larger.

After choosing n_{\max}, evaluate the independent coefficient problem for n=0,1,\ldots,n_{\max} and insert the resulting A_n into the far-field series. Truncation limits the retained partial waves but does not change the diagonal structure of the mode-wise solve.

Backscattering cross-section and target strength

Once the backscattering amplitude is known, the backscattering cross-section is:

\sigma_\text{bs} = |\mathcal{f}_\text{bs}|^2

and target strength is (MacLennan et al. 2002):

TS = 10\log_{10}\left( \frac{\sigma_\text{bs}}{1\ \mathrm{m}^2}\right).

Equivalently, TS=20\log_{10}(|\mathcal f_\text{bs}|/1\ \mathrm{m}). Within the stated boundary model, numerical approximation enters through modal truncation and special-function evaluation.

Mathematical assumptions

The spherical modal series rests on the following assumptions:

  1. Time-harmonic linear acoustics.
  2. A perfectly spherical interface.
  3. Homogeneous material properties within each region.
  4. Exact separability in spherical coordinates.
  5. Radiation condition in the exterior field.

The matched geometry and orthogonal angular basis make this solution a useful reference for more general modal and approximate models. The validation scope of the package implementation is documented on the SPHMS implementation page.

References

Anderson, Victor C. 1950. “Sound Scattering from a Fluid Sphere.” The Journal of the Acoustical Society of America 22 (4): 426–31. https://doi.org/10.1121/1.1906621.
MacLennan, David N., Percy G. Fernandes, and John Dalen. 2002. “A Consistent Approach to Definitions and Symbols in Fisheries Acoustics.” ICES Journal of Marine Science 59 (2): 365–69. https://doi.org/10.1006/jmsc.2001.1158.
Morse, Philip M., and Herman Feshbach. 1953. Methods of Theoretical Physics. McGraw-Hill.
Sommerfeld, Arnold. 1949. Partial Differential Equations in Physics. Vol. 6. Lectures on Theoretical Physics. Academic Press.