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JOURNAL OF SOUND AND VIBRATION

Journal of Sound and Vibration 300 (2007) 800–816

Analysis of airborne sound insulation and impact sound pressure level provided by a single partition containing a heterogeneity

A. Pereira, A. Tadeu

Department of Civil Engineering, University of Coimbra, Pinhal de Marrocos, 3030-290 Coimbra, Portugal Received 19 December 2005; received in revised form 7 July 2006; accepted 27 August 2006

Available online 13 November 2006

Abstract

This paper studies the acoustic behaviour provided by a single infinite elastic partition dividing an infinite acoustic medium, containing two-dimensional (2D) heterogeneities placed parallel to the layer’s surfaces, which simulate the presence of fittings such as pipes. The problem is solved in the frequency domain using the boundary element method (BEM). Only the surfaces of the heterogeneities are discretized, since 2.5D Green’s functions for the single layered media, bounded by acoustic media, are used. Time domain responses are also computed by applying a (fast) Fourier transform to the responses obtained in the frequency domain. The heterogeneities are assumed to be either rigid, free, fluid-filled or elastic-filled inclusions. The simulated models are used to study the contribution of the heterogeneities to the final airborne sound insulation and impact sound pressure level provided by a single partition. It was found that both airborne sound insulation and impact sound pressure level may be influenced by the presence of the heterogeneity at higher frequencies.

r2006 Elsevier Ltd. All rights reserved.

1. Introduction

In order to accurately predict the transmission of sound through a single separating partition a large number of variables needs to be considered. These variables include: the physical properties of the panel (mass, internal damping, elasticity modulus, Poisson’s ratio); the finiteness of the element; the mounting conditions, and the non-diffuseness of the test room. The simulation of all the acoustic phenomena involved in the sound transmission would lead to highly complex mathematical models, and so quite a number of works found in the literature adopt simplifications to deal with the problem. Among these is the well-known theoretical Mass Law, where the element is assumed to behave like a group of infinite juxtaposed masses with independent displacement and null damping forces. Sewell[1]and Sharp[2]have proposed simplified models for the frequencies below, in the vicinity of and above the coincidence effect to calculate the airborne sound insulation of single panels, improving the prediction accuracy relative to Mass Law. More recently, Tadeu et al.[3,4]developed an algorithm for predicting the airborne sound insulation provided by a single partition based on the definitions of pressure and displacement potentials, which are combined so as to verify the

www.elsevier.com/locate/jsvi

0022-460X/$ - see front matterr2006 Elsevier Ltd. All rights reserved.

doi:10.1016/j.jsv.2006.08.039

Corresponding author. Department of Civil Engineering, Polo II of the University of Coimbra, Rua Luı´s Reis Santos, 3030-788 Coimbra, Portugal. Tel.: +351 239 797 201; fax: +351 239 797 190.

E-mail address:[email protected] (A. Tadeu).

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boundary conditions at the fluid/solid interfaces. Jong-Hwa et al. [5] revisit the problem of resonant transmission related to the sound insulation of rectangular finite panels in an infinite baffle at frequencies below the critical frequency by using the general modal expansion method followed by Sewell. They investigated the validity of neglecting the resonant transmission components in the prediction of transmission loss by calculating the differences between the total transmission loss and the non-resonant transmission loss.

Alba et al.[6]revised the expression for an infinite impervious layer in a diffuse field and adjusted it in order to include the energy loss mechanisms (internal and coupling losses) produced in the layer. These authors further developed algorithms which can be used to obtain the mechanical properties of the layer with the appropriate set-up conditions, if databases are available.

Knowledge of the impact sound pressure level expected from partitions is also important at the design stage.

Although the final responses provided by the loads that act in an acoustic or in an elastic medium differ, the dynamic behaviour of partitions may be similar. Ver [7] determined a relation between airborne sound insulation and impact sound pressure level provided by partitions. Gerretsen[8]initially proposed a model to predict airborne sound insulation including flanking transmission. His model requires knowing the direct sound reduction index provided by a partition and takes into account the boundary conditions by means of a structural reverberation time and the vibration level differences across junctions, which are calculated from in situ measurements. Since a major part of the model concerns vibration transmission and radiation, he later extended it to predict impact sound pressure level [9].

Most of the works found in the literature refer to the prediction of homogeneous partitions. However, the acoustic behaviour of real partitions may be influenced by the presence of heterogeneities, which are often present inside. These may be other building elements such as heat, sewerage, drainage or water pressure pipes or pipes that host electrical cables and wires. These are not taken into account during design, and when the performance of walls is tested the results may not match the predictions. Therefore it seems important to see if the presence of those elements can influence the sound insulation of partitions. This work aims to contribute to the analysis of this problem by developing and applying a boundary element method (BEM) model to assess the acoustic behaviour of single partitions infinite in two directions (infinite plates) dividing an infinite acoustic medium. The influence of heterogeneities in the elastic partition on the acoustic behaviour is studied by determining airborne sound insulation and impact sound pressure levels. Results for a single layer solution without discontinuities are used as a reference. The algorithm uses a Boundary Element formulation where only the heterogeneity needs to be discretized, since Green’s functions for single layered media are used. These heterogeneities may be rigid, free, fluid-filled or elastic-filled inclusions. The Green’s functions’ solutions are the analytical solutions developed by Tadeu et al. [3,4]to predict airborne sound insulation provided by a single panel. The computations are performed in the frequency domain, assuming that harmonic line loads act either in the fluid or in the elastic medium. Time domain responses are then obtained by applying an Inverse Fourier Transform. Wave propagation features occurring in a single layered medium with a heterogeneity are investigated by analysing the responses provided by different sets of receivers placed in the acoustic medium.

The influence of the direction of the load on impact sound pressure level is studied. Different positions and sizes of the heterogeneity are modelled and the resulting sound level is analysed.

The next section outlines the problem formulation, indicating the Green’s functions for a single layer medium, and the BEM. Then the procedure used to calculate time domain responses is summarized. The simulations are described next, and finally the results are discussed.

2. Problem formulation

Consider an elastic layer of thickness h, infinite along its plane (x and zdirections), dividing an infinite acoustic medium, as inFig. 1. The acoustic medium has a mass densityrf, a Lame´ constantlfand permits a dilatational wave velocity af ¼ ffiffiffiffiffiffiffiffiffiffiffiffi

lf=rf

q . The material properties of the elastic medium are the density rs, Poisson’s ratio nsand a shear modulus ms. In this medium the propagation occurs following compressional waves with a velocityas¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi

2msð1nsÞ=rsð12nsÞ

p and shear waves with a velocitybs¼ ffiffiffiffiffiffiffiffiffiffiffi ms=rs

p . The internal material losses are considered by using a complex shear modulus and a complex Lame´ constant. The shear

A. Pereira, A. Tadeu / Journal of Sound and Vibration 300 (2007) 800–816 801

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modulus is computed asm¼mrð1þiZÞ, wheremrcorresponds to the classic modulus andZis the loss factor.

The Lame´ constant is written in the same form as the shear modulus.

In this paper the influence of a heterogeneity in the elastic partition on sound pressure level is studied by inserting a cylindrical circular inclusion with radius R, infinite along the zdirection, into the elastic layer.

When the system is excited by a point load oscillating with a frequencyoand acting in the acoustic medium at (x0,y0,z0), the incident pressure field at a point (x, y,z) can be obtained by the following expression:

sfull3Dðo;x;y;zÞ ¼Aei

aof aft

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi

xx0

ð Þ2þðyy0Þ2þðzz0Þ2

q

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi xx0

ð Þ2þyy02

þðzz0Þ2

q , (1)

in whichAis the wave amplitude and i¼ ffiffiffiffiffiffiffi p1

. As the geometry of the model is constant along thezdirection and the source is three-dimensional (3D), the incident field can also be obtained by calculating a series of 2D problems and applying a Fourier transformation in thezdirection. With this procedure, the responses are obtained in the frequency–wavenumber domain for varying effective wavenumbers, kaf ¼

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi o=af

2

k2z q

, with Im kaf

p0 and kzbeing the axial wavenumber. In this kz domain, the system is excited by spatially sinusoidal harmonic line loads acting at (x0,y0) whose pressure field at a point (x,y) is given by

sfullðo;x;y;kzÞ ¼iA

2 Hð Þ02 kaf

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi xx0

ð Þ2þyy02

q

eikzz. (2)

The former 3D pressure field is then calculated as a discrete summation of 2D problems obtained using expression (2), by applying an inverse Fourier transformation, and assuming the existence of an infinite number of sources placed along the z direction at equal intervals, L. This equation converges and can be approximated by a finite sum of terms. The distance L needs to be large enough to avoid spatial contamination.

The same procedure can be applied to point loads acting within the solid medium. Each 2D incident field produced by a spatially sinusoidal harmonic line load acting at a point (xs,ys) of the elastic medium can be expressed by the displacementsGi,jfull

(where the index i¼x, y, zdefines the direction in which the load is acting, while the second index, j¼x, y, z, indicates the direction of the displacement) at a point (x, y) according to the following expressions[10]:

Gfullij ðo;x;y;kzÞ ¼A k2sH0b1

rB1þg2iB2

; with i¼j¼x;y, (3)

(xs;ys;zs) αs

y (x0;y0;z0)

ρβss

αf

ρf

R Fluid Elastic

Fluid

x z

αf

ρf

Fig. 1. Geometry of the problem.

A. Pereira, A. Tadeu / Journal of Sound and Vibration 300 (2007) 800–816 802

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Gfullzz ðo;x;y;kzÞ ¼A k 2sH0bk2zB0 , Gfullxyðo;x;y;kzÞ ¼Gfullyxðo;x;y;kzÞ ¼gxgyAB2,

Gfulliz ðo;x;y;kzÞ ¼Gfullzj ðo;x;y;kzÞ ¼ikzgiAB1 with i¼j¼x;y,

where A¼1=4irso2; gx¼ ðxxsÞ=r; gy¼ ðyysÞ=r; Bn¼knbHnbknaHna; Hna¼Hð2Þn kasr

and Hnb¼ Hð2Þn kbsr

are Hankel functions of the second kind and order n; ks¼ ffiffiffiffiffiffiffiffiffiffiffi o=bs

p ; r¼

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi xxs

ð Þ2þyys2

q

; kas¼

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi o=as

2

k2z q

with Imkas

p0;kbs ¼

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi o=bs

2

k2z q

with Imkbs

p0 and kz¼ ð2p=LÞn.

In the same way, the scattered field produced by point loads with a heterogeneity inserted into the single layer can be evaluated by solving a sequence of 2D problems, with varying values ofkz.

2.1. Green’s functions for a single layered medium

This section briefly describes the procedure used to obtain the 2.5D Green’s functions for a single homogeneous elastic layer bounded by two fluid media, when excited by harmonic line loads with differentkz

values. These solutions have already been derived by Tadeu et al.[3]and can be expressed as the sum of the source terms equal to those in full space (which can be calculated according to above-defined expressions, (2) and (3)) and surface terms generated by the fluid/solid interfaces (interfaces a and b, as in Fig. 2). The calculation of the surface terms requires knowledge of the solid layer displacement potentials and the pressure potentials generated by the solid/fluid surfaces. These potentials are written as a superposition of plane waves by means of a discrete wavenumber representation (after applying a Fourier transform in thexdirection). The integrals of the expressions are transformed into a summation by considering an infinite number of virtual plane sources distributed along thexdirection at equal intervals,Lx. In the fluid medium, pressure potentials

Fig. 2. Definition of potentials, stresses and displacements at the interfaces.

Table 1

Potentials generated at the interfaces when the load acts in the elastic medium along thexdirection

Interfacea Interfaceb

Elastic medium

fx;a¼Ean¼þNP

n¼N kn nnEabAxn

Ed fx;b¼Ean¼þNP

n¼N kn nnEbbExn

Ed

cx;ax ¼0 cx;bx ¼0

cx;ay ¼Eakzn¼þNP

n¼N Eac gnBxn

Ed cx;by ¼Eakzn¼þNP

n¼N Ebc gnFxn

Ed

cx;az ¼ Ean¼þNP

n¼N

EacCxn

Ed cx;bz ¼Ean¼þNP

n¼N

EbcGxn

Ed

Fluid medium

fx;af ¼ Li

x

P

n¼þN n¼N

a2f o2lf

Ea f nfnDxn

Ed fx;bf ¼ i

Lx

P

n¼þN n¼N

a2f o2lf

Ebf nfnHxn

Ed

A. Pereira, A. Tadeu / Journal of Sound and Vibration 300 (2007) 800–816 803

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(fi;af ; fi;bf ) are defined at the interfaces, whereas in the elastic medium, the wave field is expressed by means of pressure potentials (fi;a; fi;b) and shear potentials (ci;ax; ci;ay ; ci;az ;ci;bx ; ci;by ; ci;bz ) with i¼x;y;z;f corre- sponding to the loads applied (as listed inTables 1–4).

In the expressions listed in Tables 1–4, the coefficients correspond to: Eaf ¼einfnjyj; Ebf ¼einfnjyhj; nfn¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi

k2p

f k2zk2n

q with Im nfn p0; Eab¼einjyjn ; Ebb¼einjnyhj; Eac¼eigj jny; Ebc¼eigjnyhj; gn¼

ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi k2sk2zk2n q

Table 2

Potentials generated at the interfaces when the load acts in the elastic medium along theydirection

Interfacea Interfaceb

Elastic medium

fy;a¼Ean¼þNP

n¼N

EabAyn

Ed fy;b¼ Ean¼þNP

n¼N

EbbEyn

Ed

cy;ax ¼Eakzn¼þNP

n¼N Eac

gn Cyn

Ed cy;bx ¼Eakzn¼þNP

n¼N Ebc

gn Gyn

Ed

cy;ay ¼0 cy;by ¼0

cy;az ¼Ean¼þNP

n¼N kn gnEacByn

Ed cy;bz ¼Ean¼þNP

n¼N kn gnEbcFyn

Ed

Fluid medium

fy;af ¼ Li

x

P

n¼þN n¼N

a2f o2lf

Eaf nfnDyn

Ed fy;bf ¼ Lixn¼þNP

n¼N a2f o2lf

Eb f nfnHyn

Ed

Table 3

Potentials generated at the interfaces when the load acts in the elastic medium along thezdirection

Interfacea Interfaceb

Elastic medium

fz;a¼Eakzn¼þNP

n¼N Eab nnAzn

Ed fz;b¼Eakzn¼þNP

n¼N Ebb

nnEzn

Ed

cz;ax ¼Ean¼þNP

n¼N

EacBzn

Ed cz;bx ¼ Ean¼þNP

n¼N

EbcFzn

Ed

cz;ay ¼Ean¼þNP

n¼N kn

gn EacCzn

Ed cz;by ¼Ean¼þNP

n¼N kn

gn EbcGzn

Ed

cz;az ¼0 cz;bz ¼0

Fluid medium

fz;af ¼ Lixn¼þNP

n¼N a2f o2lf

Ea f nfn

Dzn

Ed fz;bf ¼ Li

x

P

n¼þN n¼N

a2f o2lf

Eb f nfnHzn

Ed

Table 4

Potentials generated at the interfaces when the load acts in the fluid medium

Interfacea Interfaceb

Elastic medium

ff;a¼Ean¼þNP

n¼N

EabAfn

Ed ff;b¼ Ean¼þNP

n¼N

EbbEfn

Ed

cf;ax ¼Eakzn¼þNP

n¼N Eac

gn Cfn

Ed cf;bx ¼Eakzn¼þNP

n¼N Ebc

gn Gfn

Ed

cf;ay ¼0 cf;by ¼0

cf;az ¼Ean¼þNP

n¼N kn gnEacBfn

Ed cf;bz ¼Ean¼þNP

n¼N kn gnEbcFfn

Ed

Fluid medium

ff;af ¼ Li

x

P

n¼þN n¼N

a2f o2lf

Ea f nfnDfn

Ed ff;bf ¼ Lixn¼þNP

n¼N a2f o2lf

Eb f nfnHfn

Ed

A. Pereira, A. Tadeu / Journal of Sound and Vibration 300 (2007) 800–816 804

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with Im gn p0;nn¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi k2pk2zk2n q

with Imð Þnn p0;Ea¼1=2rso2Lx;Ed ¼eiknðxx0Þ;kn¼ ð2p=LxÞn;kpf ¼ o=af andkp ¼o=as. The coefficientsAin; Bin; Cin; Din; Ein; Fin; Gin; andHin with i¼x,y, z, fare unknowns which are determined by deriving the above-defined potentials in order to calculate stresses and displacements, and then establishing the appropriate boundary conditions: continuity of normal displace- ments (ui;ay ¼ui;ay;f; ui;by ¼ui;by;f) and stresses (si;ayy ¼si;a; si;byy¼si;b) and null tangential stresses (si;ayx¼0; si;ayz ¼0; si;byx¼0; si;byz ¼0) at the interfaces (seeFig. 2).

Once the unknown coefficients have been calculated, the displacements and stresses associated with the surface terms can be determined by applying partial derivatives to the potentials defined inTables 1–4. The Green’s functions for the solid/fluid formation are then obtained from the sum of the source terms and the surface terms. When this has been done, expressions for displacementsGsurfi;j , in the elastic medium are given, as follows:

Load acting in the elastic medium in thex direction:

Gsurfxx ¼Gfullxx þEa

X

n¼þN

n¼N

Axnik2n nn

Eabþ ignCxnik2z gn Bxn

Eac

EdþEa

X

n¼þN

n¼N

Exnik2n nn

Ebbþ ignGxnik2z gnFxn

Ebc

Ed,

Gsurfxy ¼Gfullxy þEa

X

n¼þN

n¼N

iknAxnEabþiknCxnEac

EdþEa

X

n¼þN

n¼N

iknExnEbbiknGxnEbc

Ed,

Gsurfxz ¼Gfullxz þEa

X

n¼þN

n¼N

ikzkn

nn

AxnEabþikzkn

gn BxnEac

EdþEa

X

n¼þN

n¼N

ikzkn

nn

ExnEbbþikzkn

gn FxnEbc

Ed. ð4Þ

Load acting in the elastic medium in they direction:

Gsurfyx ¼Gfullyx þEa

X

n¼þN

n¼N

iAynknEabþiBynknEac

EdþEa

X

n¼þN

n¼N

iEynknEbbþiFynknEbc

Ed,

Gsurfyy ¼Gfullyy þEa

X

n¼þN

n¼N

innAynEabþ ik2n

gn Bynþik2z gn Cyn

Eac

EdþEa

X

n¼þN

n¼N

innEynEbbþ ik2n

gn Fynþik2z gn Gyn

Ebc

Ed,

Gsurfyz ¼Gfullyz þEa

X

n¼þN n¼N

iAynkzEabþiCynkzEac

EdþEa

X

n¼þN n¼N

iEynkzEbbþiGynkzEbc

Ed. ð5Þ

Load acting in the elastic medium in thezdirection:

Gsurfzx ¼Gfullzx þEa

X

n¼þN

n¼N

ikzkn nn

AznEabþikzkn gn CznEac

EdþEa

X

n¼þN

n¼N

ikzkn nn

EznEbbþikzkn gn GznEbc

Ed, Gsurfzy ¼Gfullzy þEa

X

n¼þN

n¼N

ikzAznEabþiBznkzEac

EdþEa

X

n¼þN

n¼N

ikzEznEbbþiFznkzEbc

Ed, Gsurfzz ¼Gfullzz þEan¼þNX

n¼N

ik2z nn

AznEabþ ik2n

gn CznignBzn

Eac

EdþEan¼þNX

n¼N

ik2z nn

EznEbbþ ik2n

gn GnignFzn

Ebc

Ed. ð6Þ

Load acting in the fluid medium:

Gsurffx ¼Ea

X

n¼þN

n¼N

iAfnknEabþiBfnknEac

EdþEa

X

n¼þN

n¼N

iEfnknEbbþiFfnknEbc

Ed, Gsurffy ¼Ea

X

n¼þN

n¼N

innAfnEabþ ik2n

gn Bfnþik2z gn Cfn

Eac

EdþEa

X

n¼þN

n¼N

innEfnEbbþ ik2n

gn Fynþik2z gn Gfn

Ebc

Ed, Gsurffz ¼Ea

X

n¼þN

n¼N

iAfnkzEabþiCfnkzEac

EdþEa

X

n¼þN

n¼N

iEfnkzEbbþiGfnkzEbc

Ed. ð7Þ

A. Pereira, A. Tadeu / Journal of Sound and Vibration 300 (2007) 800–816 805

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