“Porous layer” here stands for any homogeneous, isotropic material with characteristic propagation constant \(\Gamma _{a}\) and wave impedance \(Z_{a}\). If the material is air, then \(\Gamma _{a}\to jk_{0}\); \(Z_{a}\to Z_{0}\).
Sound incidence is as in → Sect. D.1 .
Sound field above absorber: p\({}_{{1}}\)=p\({}_{{i}}\)+p\({}_{{r}}\) (as in → Sect. D.1 )?,
sound field in absorber: \(p_{2}(x,y)=p_{t}(x,y)=B\cdot e^{{\scriptsize-\Gamma _{a}\left({x\cos\Theta _{a}+y\sin\Theta _{a}}\right)}}\)?. (1)
The boundary conditions are:
•?Equal propagation constant in y direction on both sides;
•?Equal normal admittance component on both sides (is equivalent to matching sound pressure and normal particle velocity).
Refracted angle \(\Theta\) \({}_{{a}}\) (complex!): \(\displaystyle\frac{\sin\Theta _{a}}{\sin\Theta}=\displaystyle\frac{j\, k_{0}}{\Gamma _{a}}\)?. (2)
Reflection factor r: \(\displaystyle r=\frac{Z_{a}/\cos\Theta _{a}-Z_{0}/\cos\Theta}{Z_{a}/\cos\Theta...
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(2008). Plane Wave Reflection at an Infinitely Thick Porous Layer. In: Mechel, F.P. (eds) Formulas of Acoustics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-76833-3_49
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