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Multiscale modeling of acoustic shielding materials

Citation for published version (APA):

Gao, K., Dommelen, van, J. A. W., & Geers, M. G. D. (2014). Multiscale modeling of acoustic shielding materials. Poster session presented at Mate Poster Award 2014 : 19th Annual Poster Contest.

Document status and date: Published: 01/01/2014 Document Version:

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Background

Acoustic shielding is very important for high-tech sys-tems and in human life. Porous materials like acoustic foams can be used to improve the shielding performance and their absorption abilities depends on the interac-tion of the acoustic wave and the complex microstruc-ture. These effects are captured in a multiscale model for the porous material.

Figure 1: Microstructure of an acoustic foam obtained from scanning electron microscopy (left) and X-ray computed tomography (right).

Framework

As illustrated in Figure2, the macroscopic problem is de-scribed by the solid displacementus

M and the air

pres-surepfM. The associated macroscopic gradients are pre-scribed on the boundary of the linearized microscopic Representative Volume Element (RVE). The homogenized solid stressσs

M and air displacementu f

M are calculated

based on the energy consistency.

Macroscopic Problem fsM− ∇M· (σsM) T = 0 fM− ∇M· ufM = 0 Solid Fluid Microscopic RVE fs M, σsM ufM, fM continuous interface us M,∇MusM ∇MpfM, p f M

Figure 2: The homogenization framework of sound propagation in a deformable porous material.

Simulation

A macroscopic sound absorption test on a porous layer is conducted as shown in Figure 3 and there are two models: (a) anisotropic Biot’s equations with the param-eters obtained from the homogenization approach and (b) modification fully based on the homogenization ap-proach.

Figure 3: Sound absorption test of the porous material with the RVE in Figure2.

The results is compared with a reference of direct numer-ical simulation (DNS). It can be found that the resonance frequency predicted by Biot’s equations is higher than the DNS, whereas the modification gives a better result. The deviation at high frequency can be due to the intrin-sic limitation of the homogenization approach because the wavelength becomes close to the characteristic pore size at high frequency so that the scale separation is not well satisfied. 0 1000 2000 3000 4000 5000 0.0 0.2 0.4 0.6 0.8 1.0 S o u n d A b s o r p t i o n C o e f f i c i e n t [ -] Frequency [Hz] DNS Biot-Homogenization Modification 0 1000 2000 3000 4000 5000 0 1 2 3 4 5 A B S (Z / Z 0 ) [-] Frequency [Hz] DNS Biot-Homogenization Modification 0 1000 2000 3000 4000 5000 -0 A R G ( Z /Z 0 ) [ ra d ] Frequency [Hz] DNS Biot-Homogenization Modification

Figure 4: Comparisons of normal incident sound absorption coeffi-cients (left figure) and the surface impedances (right figures).

Conclusions & future work

The homogenization framework gives a good description of the sound propagation problem in the porous mate-rial. The next step is to consider realistic microstructure based on the X-ray computed tomography technique.

Multiscale modeling of acoustic

shielding materials

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