CA05 exercise · Radiation and BEM-preparation exercise

Rayleigh Integral Plate Radiation

Discretise a baffled vibrating plate into constant-velocity patches, evaluate a Rayleigh-integral pressure estimate and interpret radiation indicators such as coincidence frequency.

60–90 minLinked to Boundary Element Method for Acoustic RadiationDashboard progress enabled

Aim

Radiation from a baffled vibrating plate

This exercise connects structural velocity from CA04 to acoustic radiation in CA05. You approximate a vibrating plate by small patches and sum their Rayleigh-integral contributions at receiver points.

1

Explain the boundary-only idea

BEM and Rayleigh-integral models do not mesh the full exterior air volume. Instead, they use boundary or surface data, such as normal velocity, to evaluate radiated pressure.

Which input is most directly used by the Rayleigh integral for a baffled vibrating plate?

2

Compute patch area and coincidence frequency

For a 1.0 m × 0.6 m plate discretised by 20 × 12 patches, compute the area of one patch. For an aluminium plate with h = 3 mm, estimate the coincidence frequency.

Python exercise

Run the patch-based Rayleigh integral

The Python code discretises the plate into patches and plots the pressure field in a plane above the plate.

Expected observation

The pressure field should be strongest above the vibrating plate and show spatial variation due to interference between patch contributions.

Teaching note

This is a teaching-level radiation calculation. A production BEM model requires singular integration, proper boundary conditions and validation.

Written submission

Radiation interpretation

Vibration versus radiation

Why can a structure vibrate strongly but radiate weakly?

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