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VRIJE UNIVERSITEIT BRUSSEL Acoustics - the Dept. of ...

VRIJE UNIVERSITEIT BRUSSEL Acoustics - the Dept. of ...

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4.2. REALIZATION OF ACOUSTIC ABSORPTION 69Thenarrower<strong>the</strong>poresare,<strong>the</strong>strongerwillbe<strong>the</strong>airfriction, thus<strong>the</strong>stronger <strong>the</strong> damping, i.e. absorption. In order to measure <strong>the</strong> acousticabsorption <strong>of</strong> a porous material an experiment can be conducted tomeasure <strong>the</strong> airflow through <strong>the</strong> material as shown in Figure 4.6. Thespecific air resistivity R s is a measure for this, defined by R s = −1vIt seems obvious that R s must be sufficiently large to achieve dampingand thus absorption. On <strong>the</strong> o<strong>the</strong>r hand R s should not be too large,because<strong>the</strong>n<strong>the</strong>poreswillbecometoonarrowandonlyasmallfraction<strong>of</strong> <strong>the</strong> incident intensity will penetrate, while <strong>the</strong> main part is reflected.The layer thickness is also an important parameter. Indeed, in orderto get a damped wave, it must penetrate a sufficient distance into <strong>the</strong>porous material. Moreover, <strong>the</strong> damping is proportional to <strong>the</strong> wavevelocity (and not <strong>the</strong> pressure) which has a maximum at a quarterwavelength away from <strong>the</strong> wall. One thus comes to <strong>the</strong> conclusionthat relatively low R s and relatively thick material should give rise t<strong>of</strong>avorable absorption properties. One should especially not think thathigh R s and small thickness give rise to good absorption. This cheapsolution leads to bad results.Frequency also plays a major role here, since <strong>the</strong> particle velocity dependson it. The friction losses, which are dependent on <strong>the</strong> viscosity,increase with increasing speed, thus increasing frequency <strong>of</strong> sound.Hence porous layers especially absorb high frequencies. Fur<strong>the</strong>r, onemayalso imaginethatalargelayer thickness isrequired toabsorblowerfrequency (large wavelength).The pore structure also plays a role (granular or fibrous material ...).The structure can be described by means <strong>of</strong> <strong>the</strong> so-called tortuosity(this is <strong>the</strong> randomness with which <strong>the</strong> fibers are arranged in <strong>the</strong> material).The method <strong>of</strong> fixation in front <strong>of</strong> <strong>the</strong> wall. If fixed on pr<strong>of</strong>iles, a fewcentimeters infront<strong>of</strong>ahardwall, <strong>the</strong>noneobtainsanabsorbenteffect,approximately equivalent to that <strong>of</strong> a layer absorbent material, equallyto <strong>the</strong> sum <strong>of</strong> <strong>the</strong> thickness <strong>of</strong> <strong>the</strong> air layer and <strong>the</strong> thickness <strong>of</strong> <strong>the</strong>absorbent material.Caution: paint covers <strong>the</strong> fine pores and annihilates <strong>the</strong> sound-absorbingeffect <strong>of</strong> porous materials (<strong>the</strong>re is no danger with large pores).Some numerical values <strong>of</strong> <strong>the</strong> specific flow resistivity : R s = 10 4 for glasswooland rockwool, R s = 10 5 for compact glasswool and compact rockwoolR s = 10 6 for compact fiberboard and R s = 10 7 for compact stony materials.∂p. ∂x

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