Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 78 1 Solution Created 2026-10-03 Updated 2026-10-14
Let use the Heaviside step function, and , so that points from the body into the fluid. The kinematic boundary condition gives on the surface. In the exterior, mass conservation and the Euler equations for an inviscid fluid areProducts with are understood distributionally, using and . With , the extended continuity equation isThe corresponding extended momentum equation isbecause its advective surface term is . Differentiate continuity in time and substitute the divergence of momentum. Subtracting gives the Ffowcs Williams-Hawkings equationwhere the inviscid Lighthill stress tensor isIf denotes total pressure, this tensor includes the constant ambient pressure . Its contribution cancels the corresponding surface term exactly. For radiation integrals it is convenient to subtract from both terms, making with . The displayed source identity is unchanged by this consistent pressure-gauge subtraction.
Assume no incoming sound and no free initial acoustic field. Put , , , and . Convolution with the retarded acoustic Green function gives the three source integrals, for an observer outside the body:These are the surface thickness, surface loading and volume quadrupole contributions. The retarded surface Dirac delta distributions must remain inside the integrals: integrating them over a moving retarded surface produces the moving-surface retarded Jacobian, and is not generally the same as simply substituting one retarded time into an instantaneous surface integral.
For an acoustic compact-source approximation, suppose the dominant sources have size , source frequency scale , and . Also require and the acoustic far field . Then , , and the leading source integrals use the common time . Slow source motion relative to is implicit in this leading retardation approximation. DefineThus is net displaced mass per unit time, is the fluid pressure force on the body, and is the integrated excess Lighthill stress tensor. The minus sign in fixes the requested loading convention; the force on the fluid is opposite. On the radiating terms, , givingSpatial derivatives of produce near-field terms of orders and , omitted here. Neglecting source delays is a separate approximation from discarding those observer near-field terms. If a leading integrated source vanishes by symmetry, its first nonzero delay correction can be as important as another retained multipole.
For the translating sphere, write its center as , with a unit vector, and its velocity as . Let , and . Impermeability gives . Since its volume is constant,in the leading compact formula. The individual local thickness sources have scale , but their net monopole cancels.
At first order in amplitude and leading order in , the exterior incompressible velocity potential is , where is measured from the mean center. It has at . Linear Bernoulli equation gives there. Since ,This is the added mass of a sphere. The explicit leading loading contribution isIt scales as . In homentropic small-amplitude flow the volume stress is quadratic to leading order, over volume , so the volume acoustic quadrupole has scaleIt is smaller than the linear dipole by and can contain a second harmonic.
For completeness, the exact thickness-source integral has a nonzero first delay correction even though . Its first spatial moment isExpand its integrand at . The leading nonzero translating-sphere acoustic thickness dipole is thereforeIt too scales as . Thus zero net-volume monopole does not mean zero thickness radiation. The full leading linear sound, summing thickness and loading, isThe leading compact equation gives the requested zero and added-mass terms; this extra delay calculation is necessary to obtain the complete linear field when its nominal monopole has cancelled.