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Articles

Improved integral formulae for supersonic reconstruction of the acoustic field

Pages 898-924 | Received 24 Mar 2017, Accepted 15 Aug 2017, Published online: 08 Sep 2017

Abstract

In this work we derive surface integral formulae for the frequency dependent power operator in arbitrary geometries. This operator is combined with layer representations and measured pressure (or normal velocity) near-field holograms to construct a non-negative intensity distribution quantifying the areas of the vibrating structure that produce radiation to the far-field. It is demonstrated that the sound producing regions of the structure are clearly revealed using the derived formulae and that the spatial resolution is limited to a half-wavelength. We validate our methodology using numerically generated data that corresponds to the excitation of an elastic spherical shell by a point force.

AMS Subject Classifications:

1. Introduction

1.1. Overview

By virtue of their interaction with the fluid boundary, vibrating structures emit a sound that often we would like to reduce. The level of the emission from a structure is quantified by the radiated acoustic power, computed from the integral over its vibrating surface of the normal acoustic intensity. The location of unwanted sources of sound on the structure is identified from large values of surface intensity especially when it is not highly bipolar (positive and negative), that is, when there is a minimum circulation of power flow in and out of the structure. Most vibrating structures of interest exhibit a highly bipolar intensity and thus it is very difficult to locate hot spots of radiation in an effort to control the vibrator.

Array measurements that consist of microphones (or velocity probes) sampling the fields simultaneously at a spatially distributed set of points are common in acoustics. Array measurements are ideal for beamforming, very common in the acoustic measurement industry which is often used to locate sources in space. Although intensity arrays also exist providing a direct measurement of the intensity at each sensor location, there are elegant mathematical formulations that allow for an indirect measurement of the intensity based on the distributed measurement of the pressure/velocity fields acquired from arrays with pressure/velocity probes. For example, for separable surfaces of the wave equation (planes, spheres or cylinders), the field has a spectral eigenfunction decomposition that allows the localization of sources on the vibrator. One such method is near-field acoustical holography (NAH) [Citation1]. Similarly this decomposition can be explicitly used to the localization of hot spots by minimizing the bipolar nature of the intensity field. This approach is known as supersonic intensity (SSI) [Citation2,Citation3]. The SSI technique has been used extensively to locate the radiation sources on naval ships with great success.

Although the previous approaches are powerful, they have been developed only for geometries that allow the analytical spectral eigenfunction decomposition. Recently it has been shown that SSI could be formulated in a planar geometry as a spatial convolution with a known kernel [Citation4,Citation5] avoiding the need for Fourier transforms, yielding direct insight into the SSI method due to knowledge of the analytical form of the convolution kernel (first order Bessel function). There have been other methodologies for arbitrarily shaped geometries that use boundary elements methods (BEM) discretizations combined with a spectral cut of the singular value decomposition [Citation6Citation8]. Although proven efficient in certain conditions, the spectral cut is based on ad-hoc rules. Another approach uses the explicit representation of the impedance matrix to produce a non-negative intensity quantity [Citation9]. There are many promising aspects of this approach, but the calculation of the explicit matrix representation can be computationally expensive. Recently in [Citation10] we introduced an approach based on the calculation of the power operator for the single layer representation, which utilizes spectral cut to estimate the SSI. The ideas of this paper were improved in our recent work [Citation11], where we developed an explicit integral formula of the power operator that produces a non-negative intensity.

In this work we extend the previous theoretical results in [Citation11]. In Section 2 we expand the power operator integral representation for the double and combined layer representation. The corresponding non-negative intensity representation is shown in Section 3 with corresponding reconstructions for numerically generated point sources data. Finally in Section 4 we validate all the non-negative intensity methodologies using data from a spherical elastic shell excited by a point force.

1.2. Integral representations of radiating waves

Assume that Ω represents a complex vibrating structure in a fluid and Ω+:=R3\Ω¯ is connected. Denote as Γ the corresponding boundary of Ω, Ω0 a bounded domain that contains Ω¯ and let Γ0 be its corresponding boundary (see Figure ). For a steady-state acoustic wave p its radiating behavior in an homogeneous medium is modeled by the Helmholtz equation(1) Δp+k2p=0,inΩ+,limrrrp-ikp=0,r=|x|,x^=x/r,(1)

where x=(x1,x2,x3), k=ω/c is the wave number, ω the angular frequency and c is the speed of sound in the medium.

Figure 1. Setup for exterior radiation problem.

Figure 1. Setup for exterior radiation problem.

The classical representation of a radiated acoustic wave (known as the Direct formulation) uses the Helmholtz–Kirchhoff integral equation [Citation12](2) p(x)=Kp(x)-iωρSVn(x),xΩ+,(2)

where Vn denotes the normal velocity. Here we follow the notation of [Citation13], for the single and double layer operators S and K given by(3) Sφ(x):=ΓΦ(x,y)φ(y)dS(y),Kφ(x):=ΓΦ(x,y)ν(y)φ(y)dS(y),(3)

and the normal derivative operators K and T given by(4) Kφ(x):=ΓΦ(x,y)φ(x)dS(y),Tφ(x):=ν(x)ΓΦ(x,y)ν(y)φ(y)dS(y),(4)

where(5) Φ(x,y)=expik|x-y|4π|x-y|,(5)

is the free space radiating fundamental solution to the Helmholtz equation. In (Equation3) and (Equation4) ν is the outward unit normal and in (Equation2) ρ is the medium density. As in [Citation13] there are jump relations when xΓ(6) Kφ+(x):=ΓΦ(x,y)ν(y)φ(y)dS(y)+12φ(x),Kφ+(x):=ΓΦ(x,y)ν(x)φ(y)dS(y)-12φ(x),(6)

where the superscript sign ‘+’ is used to denote that xΓ is the limiting value of the sequence of points {ym}Ω+.

As an alternative to representation (Equation2), we found representations to (Equation1) that use individual layers (known as the indirect formulations) like the single layer representation (see [Citation14Citation16])(7) p(x)=Sφ(x),xΩ+,(7)

or the double layer representation (see [Citation17,Citation18])(8) p(x)=Kφ(x),xΩ+.(8)

In (Equation7) and (Equation8), φ is the surface density function. When k2 is a Dirichlet eigenvalue of the Laplace operator in Ω then it is known that there is no unique φ such that the single layer representation in (Equation7) holds. A similar situation is found for the double layer representation in (Equation8) when for k2 a Neumann eigenvalue of the Laplace operator in Ω. This situation is avoided using combined representation [Citation13] (also known as the Burton-Miller representation [Citation19] in the acoustic literature)(9) p(x)=Kφ(x)-iηSφ(x),xΩ+,(9)

for a positive constant η.

1.3. Radiation theory

The classical structural acoustic theory (see [Citation1,Citation20]) assumes that the radiating sound pressure p results from the interaction between the structure vibration Vn and the normal derivative of the acoustic pressure νp. This interaction is modeled by Euler’s equation(10) Vn(x)=1iρωνp(x),xΓ.(10)

The acoustic pressure p is given in Nm-2 units and the normal velocity Vn in ms-1 units. The total power (given in units of W) that radiates from the surface Γ, for the wave p, is given by(11) Π(Γ,p):=ΓI(x)dS(x),(11)

where the normal intensityI(x):=12Rep(x)Vn(x)¯,xΓ,

is a power density quantification (with units of Wm-2) over the surface of the vibrating structure Γ.

In this work we are interested in the inverse problem of wave continuation [Citation21] or NAH [Citation22]. For this inverse problem we use acoustic sensors located over the surface Γ0 which (ideally) is close and conformal to the vibrating structure Γ. The goal of this problem is to reconstruct the complete acoustic field (pressure, velocity and intensity) at the surface Γ from the measurements at Γ0. The classical methodology of solution requires that the field p is represented by an integral boundary layer, so the inverse problem is reduced to the reconstruction of the surface density φ for the corresponding integral equation over xΓ0. Then the corresponding acoustic field at Γ uses the density φ with the corresponding surface layer (and jump relation) (see [Citation16] for more details). The single layer representation (Equation7) uses the resultant density φ to obtain the field(12) p(x)=Sφ(x),Vn(x)=1iρωKφ+(x).(12)

Similarly the double layer representation uses the resultant density φ to obtain(13) p(x)=Kφ+(x),Vn(x)=1iρωTφ(x).(13)

Finally the combined layer approach use the density to obtain(14) p(x)=Kφ+(x)-iηSφ(x),Vn(x)=1iρωTφ(x)-iηKφ+(x).(14)

Given the layer representation (Equation7), (Equation8) or (Equation9) of the acoustic wave p, the radiated power is given by(15) Πk(Γ,φ)=Γφ(x)Pφ(x)¯dS(x),(15)

where P is known as the power operator [Citation11]. From this representation, we have the explicit expression for the normal intensity(16) I(x):=φ(x)Pφ(x)¯.(16)

The normal intensity shows the distribution of the acoustic energy at the radiating surface. A positive value of the intensity means energy leaving the surface Γ (in direction of the normal), while negative values means energy entering the structure (in opposite direction of the normal).

For the single layer representation (Equation7) we denote the power operator in (Equation15) as Ps and the corresponding intensity Is. Similar notations for the representations (Equation8) or (Equation9) for the power operator will be Pd or Pc respectively and the intensity as Id or Ic. As explained in [Citation11] the intensity reconstructions from the NAH technique will contain complex combinations of negative and positive values. In Sections 2 and 3 we provide explicit integral representations of Ps, Pd, Pc and a proof that the corresponding operators are positive definite. These results allows to create an expression for the ‘non-negative’ intensity(17) Iss(x):=P1/2φ(x)2,(17)

for the power operator P (which can be Ps, Pd or Pc) and the upper script denotes the square root of the operator. We will show that the expression for the non-negative intensity matches total power, providing an expression for the SSI.

2. Power operator representations

2.1. Mathematical preliminaries

A Lipschitz surface Γ, means that Γ is locally the graph of a Lipschitz function. A surface Γ is Cr,1 if is a locally graph of functions where the rth derivative is Lipschitz. We will assume that Γ:=Ω is a Lipschitz boundary, which means that Γ is locally the graph of a Lipschitz function. We will consider only Ω with connected Ω+. Recall that H(s)(Ω) denotes the Sobolev space of functions on Ω whose partial derivatives up to order s are square integrable and .(s) denotes the standard norm in this space. Similarly Hloc(s)(Ω+) denotes the space of functions that are H(s)(B\Ω¯) for every ball B that contains Ω¯. We let .2=.(0) be the norm in the space L2(Ω).

Finally we define the inner product between trace functions fH(s-1/2)(Γ) and gH(s+1/2)(Γ)f,gΓ:=Γf(x)¯g(x)dS(x)

with s(-1/2,1/2).

We will use the following useful results that can be found in the acoustic literature. Assume that pHloc(1)(Ω+) is a solution to the Helmholtz Equation (Equation1) with k>0 and Sommerfeld radiation conditions (Equation1). For the following lemmas let Ω0 be a bounded domain with Lipchitz boundary. Assume that Ω0 contains Ω¯. We denote as Br the ball with center in the origin and radius r>0. Similarly Γr is the boundary of Br. For the following result we will utilize the spherical harmonics, which are defined as(18) Ynm(x^):=2n+14π(n-m)!(n+m)!Pnm(cosθ)exp(imϕ),(18)

for n=0,1,2, and m=0,±1,±2,±n, where x^=(cosϕsinθ,sinϕsinθ,cosθ) and Pnm is the associated Legendre function. It is well known that the spherical harmonics form an orthonormal basis at the surface of the unit sphere S2, moreover at ΓrYnm,YnmΓr=r2δnnδmm,

where δ is the Kronecker delta function. The radiating solution p can be represented in R3\Br (see [Citation23])(19) p(x)=n=0m=-nnAnmhn(k|x|)Ynm(x^),(19)

where hn is the spherical Hankel function of the first kind. This representation yields the explicit expression for the power (see [Citation1, Chapter 6])(20) Πk(Γr,p)=12Re1iρωrp,pΓr=12ρωkn=0m=-nn|Anm|2.(20)

In the remaining section, we will not make the distinction using the superscript ‘+’ when the layers are evaluated at xΓ to simplify the notation. The following Lemma follows from [Theorem 7.1,7.2][Citation24]

Lemma 2.1:

For -1/2<s<1/2, we have the following mapping properties(21) S:=H(s-1/2)(Γ)H(s+1/2)(Γ),K:=H(s-1/2)(Γ)H(s-1/2)(Γ),K:=H(s+1/2)(Γ)H(s+1/2)(Γ),T:=H(s+1/2)(Γ)H(s-1/2)(Γ),(21)

If Γ is of class Cr+1,1 for an integer r0, then (Equation21) holds for -r-1sr+1.

Notice that S, and T are self-adjoint operators, while K=K. This will be used in the following result

Assume φ1H(1/2), φ2H(-1/2), then we have the operator representation(22) p(x)=Kφ1(x)-iηSφ2(x),(22)

where η>0.

Lemma 2.2:

The representation in (Equation22) satisfies the Helmholtz Equation (Equation1) in Ω+. Moreover pHloc(1)(Ω+) and(23) ReVn,pΓ=Re1iρωTφ1,Kφ1Γ+η2Re1iρωKφ2,Sφ2Γ-ηIm1iρωKφ2,Kφ1Γ+ηIm1iρωTφ1,Sφ2Γ.(23)

Proof It’s trivial to show that the representation (Equation22) solves (Equation1). From [Theorem 7.1][Citation24] we have thatS:H(-1/2)(Γ)Hloc(1)(Ω+),K:H(1/2)(Γ)Hloc(1)(Ω+)

which yields that pHloc(1)(Ω+) and the Euler’s equation yields thatVn(x)=1iρωTφ1(x)-iηKφ2(x).

Finally we use this relation to obtain (Equation23).

Theorem 2.3:

For -1/2<s<1/2, the single layer representation (Equation7) with φH(s-1/2)(Γ)-pagination yields the power operator Ps:H(s-1/2)(Γ)H(s+1/2)(Γ) with the operator representation(24) Ps=14iρωSK-KS.(24)

The double layer representation (Equation8) with φH(s+1/2)(Γ) yields the power operator Pd:H(s+1/2)(Γ)H(s-1/2)(Γ) with operator representation(25) Pd=14iρωKT-TK.(25)

Given Γ is of class C1,1 the combined representation (Equation9) with φH(1/2)(Γ) yields the power operator Pc:H(1/2)(Γ)H(-1/2)(Γ) with the operator representation(26) Pc=Pd+η2Ps-Psd+Pds,Psd=14ρω(K)K+KK,Pds=14ρωTS+ST.(26)

Proof The result for Ps is found in [Citation11]. For φH(s+1/2)(Γ)2Re1iρωTφ,KφΓ=φ,1iρωTKφΓ+φ,1iρωKTφΓ

From Lemma 2.1 we obtain that the operators TK and KT map H(s+1/2)(Γ) to H(s-1/2)(Γ), then (Equation25) follows.

Finally for φH(1/2)(Γ), Lemma 2.2 yields2Re1iρωTφ-iηKφ,Kφ-iηSφΓ=2η2Re1iρωKφ,SφΓ+2Re1iρωTφ,KφΓ-2ηIm1iρωKφ,KφΓ+2ηIm1iρωTφ,SφΓ.

From Lemma 2.1 the operators (K)K, KK, TS, and ST map H(1/2)(Γ) to H(1/2) then2iIm1iρωKφ,KφΓ=-1iρωφ,(K)K+KKφΓ,2iIm1iρωTφ,SφΓ=-1iρωφ,TS+STφΓ,

which yields (Equation26).

Lemma 2.4:

For φH(1/2)(Γ) the double layer representation (Equation8) yields(27) 12Re1iρωTϕ,KϕΩ0=ϕ,PdϕΓ,(27)

where the power operator is defined as the integral operatorPdϕ(x)=Ω0Υd(x,y)ϕ(y)dS(y)

where(28) Υd(x,y)=Ω0141iρωΦ(z,x)ν(z)ν(x)Φ(z,y)ν(y)¯+1iρωΦ(z,y)ν(z)ν(y)¯Φ(z,x)ν(x)dS(z).(28)

Proof Using the double layer representation (Equation8), we can change the order of integration to obtain the relation1iρωTφ,KφΩ0=Ω01iρωTφ(x)¯Kφ(x)dS(x)=Ω0ΓΓ1iρωΦ(x,y)ν(x)ν(y)¯φ(y)¯Φ(x,z)ν(z)φ(z)dS(z)dS(y)dS(x)=Γφ(z)Γφ(y)¯Ω01iρωΦ(x,y)ν(x)ν(y)¯Φ(x,z)ν(z)dS(x)dS(y)dS(z)=Γφ(z)Γφ(y)Ω01iρωΦ(x,y)ν(x)ν(y)Φ(x,z)ν(z)¯dS(x)dS(y)¯dS(z).

Changing variables and the order of integration, we obtain the first equation from (Equation28).

Lemma 2.5:

For φH(1/2)(Γ) the combined layer representation (Equation9) yields(29) 12Im1iρωKφ,KφΩ0=φ,PsdφΓ,12Im1iρωTφ,SφΩ0=φ,PdsφΓ,(29)

were the operators Psd and Pds are defined as integral operatorsPsdφ(x)=Ω0Υsd(x,y)φ(y)dS(y),Pdsφ(x)=Ω0Υds(x,y)φ(y)dS(y)

where(30) Υsd(x,y)=Ω014i1iρωΦ(z,x)ν(z)Φ(z,y)ν(y)¯-1iρωΦ(z,y)ν(z)¯Φ(z,x)ν(x)dS(z),Υds(x,y)=Ω014i1iρωΦ(z,x)ν(z)ν(x)Φ(z,y)¯-1iρωΦ(z,y)ν(z)ν(y)¯Φ(z,x)dS(z).(30)

Proof We proceed as in the previous lemma, so the relations1iρωKφ,KφΩ0=Γφ(z)Γφ(y)Ω01iρωΦ(x,y)ν(x)Φ(x,z)ν(z)¯dS(x)dS(y)¯dS(z)

and1iρωTφ,SφΩ0=Γφ(z)Γφ(y)Ω01iρωΦ(x,y)ν(x)ν(y)Φ(x,z)¯dS(x)dS(y)¯dS(z)

yield (Equation30).

2.2. Representation formulas on an infinite medium

For the following theorem we use the result given in Chapter 7 of [Citation25](31) j0k|x-y|=4πn=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^),(31)

where j0(t)=sin(t)/t is the spherical bessel function.

The following Theorem can be found in [Citation11].

Theorem 2.6:

The single source representation (Equation7) for a density φH(-1/2)(Γ) yields the integral representation of the power operator in (Equation15)(32) Psφ(x):=18πρcΓφ(y)j0k|x-y|dS(y)(32)

Theorem 2.7:

The double source representation (Equation8) for a density φH(1/2)(Γ) yields the integral representation of the power operator in (Equation15)(33) Pdφ(x):=18πρcΓφ(y)2j0(k|x-y|)ν(x)ν(y)dS(y)(33)

Proof Assume that Br is a ball with radius r>0 such that Ω¯Br then [Citation11, Lemma 2.1] and Lemma 2.4 yield thatΠkΓ,φ=ΠkΓr,φ=12Re1iρωTφ,KφΓr=φ,PdφΓr

Set |z|=r, then notice that |z|>|x| and |z|>|y| then we have the representationΦ(z,x)ν(z)ν(x)=ik3ν(x)·x|x|n=0m=-nnjn(k|x|)Ynm(x^)¯hn(k|z|)Ynm(z^),Φ(z,y)ν(y)=ik2ν(y)·y|y|n=0m=-nnjn(k|y|)Ynm(y^)¯hn(k|z|)Ynm(z^).

We use these decomposition over the integral representation of Υd(x,y) in (Equation28) to obtainΓr1iρωΦ(z,x)ν(z)ν(x)Φ(z,y)ν(y)¯dS(z)=-ir2k5ρων(x)·x|x|ν(y)·y|y|×n=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^)hn(k|z|)hn(k|z|)¯

andΓr1iρωΦ(z,y)ν(z)ν(y)¯Φ(z,x)ν(x)dS(z)=ir2k5ρων(x)·x|x|ν(y)·y|y|×n=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^)hn(k|z|)¯hn(k|z|)

Since hn(t)¯hn(t)=1t2-i+O1t (see [Citation11]) and r can be arbitrarily large, we let r thenΥs(x,y)=limrir2k54ρων(x)·x|x|ν(y)·y|y|×n=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^)hn(kr)¯hn(kr)-hn(kr)hn(kr)¯=k32ρων(x)·x|x|ν(y)·y|y|n=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^)

Finally we use (Equation31) to obtain (Equation33).

Theorem 2.8:

The combined layer representation (Equation9) for a density φH(1/2)(Γ) and any η>0, yields the integral representation of the power operator in (Equation15)(34) Pcφ(x):=18πρcΓφ(y)2j0(k|x-y|)ν(x)ν(y)+η2j0(k|x-y|)dS(y).(34)

Proof As in Theorem 2.7 we have thatΠk(Γ,φ)=12η2Re1iρωKφ,SφΓr+12Re1iρωTφ,DφΓr-12ηIm1iρωKφ,DφΓr+12ηIm1iρωTφ,SφΓr

Assume that |z|=r, then notice that |z|>|x| and |z|>|y| then we have the representationΦ(z,x)ν(z)=ik2n=0m=-nnjn(k|x|)Ynm(x^)¯hn(k|z|)Ynm(z^),Φ(z,y)ν(y)=ik2ν(y)·y|y|n=0m=-nnjn(k|y|)Ynm(y^)¯hn(k|z|)Ynm(z^).

Using the integral representation of Υsd(x,y) in (Equation30), as in the previous theorem, we obtainΥsd(x,y)=-r2k44ρων(y)·y|y|×n=0m=-nnjn(k|x|)jn(k|y|)Ynm(x^)¯Ynm(y^)hn(kr)¯hn(kr)+hn(kr)hn(kr)¯.

Since r is arbitrarily and Re{hn(t)¯hn(t)}=O1t3 then Υsd(x,y)=0 as r. In a similar way we can also prove that Υds(x,y)=0.

Then we have the expressionΠk(Γ,φ)=12Re1iρωTφ,DφΓr+12η2Re1iρωKφ,SφΓr.

Finally using the results from previous theorems we can prove formula (Equation34).

Notice that(35) 2j0(k|x-y|)ν(x)ν(y)=kν(x)·ν(y)j1(k|x-y|)|x-y|-3kν(x)·(x-y)|x-y|ν(y)·(x-y)|x-y|j1(k|x-y|)|x-y|+k2ν(x)·(x-y)|x-y|ν(y)·(x-y)|x-y|j0(k|x-y|).(35)

Since j1(t)/t1/3 as t0 then integral kernel formulas in (Equation33), (Equation34) defines a function continuous when x=y.

The following corollary results from the techniques used to obtain Theorem 2.8

Corollary 2.9:

The Helmholtz–Kirchhoff formula in (Equation2) yields the expression for the power(36) Πk=p,PdpΓr+(ρω)2Vn,PsVnΓr.(36)

Corollary 2.10:

Assume that Γ is of class C1,1. The power operator Ps:L2(Γ)L2(Γ) is a compact positive definite operator. If k is not a Dirichlet eigenvalue of Ω then Ps is strictly positive. The power operator Pd:H(1/2)(Γ)H(-1/2)(Γ) is a positive definite operator. If k is not a Neumann eigenvalue of Ω then Pd is strictly positive. The power operator Pc:H(1/2)(Γ)H(-1/2)(Γ) is a strictly positive definite operator.

Proof The proof for Ps can be found in [Citation11]. Lemma 2.4 in [Citation11] yields that the power operators Pd, Pc are positive definite. When k is not a Neumann eigenvalue, the uniqueness of the double layer representation guarantees that the operator is strictly positive definite. Finally since the combined representation is unique for any k>0 then Pc is a strictly positive definite operator.

Figure 2. Half space radiation problem.

Figure 2. Half space radiation problem.

2.3. Representation formulas on a half-space medium

In the previous subsection we focus our analysis of the power operator in an infinite medium. For many acoustical applications it will be a substantial simplification to assume predefined interface conditions over a medium. Let consider the information of the problem be given over R+3 and ΩR+3 then we denote Ωh=R+3Ω, Ωh+=R+3\Ωh and Γh=Ωh (see Figure ).

The boundary layer operators (Equation3) and (Equation4) over Ωh+ are defined by replacing the fundamental solution Φ by the half-space solution(37) Φh(x,y)=expik|x-y|4π|x-y|+hexpik|x-y|4π|x-y|,y=(y1,y2,-y3).(37)

The function Φh is the fundamental solution to the half-space Helmholtz equation with h=-1 for sound-soft interface or h=1 sound-hard interface. The sound soft condition is generally used for underwater problems where we assume that the pressure field is 0 at the air-water interface. Similarly the sound hard condition is used when we assume that the object is laying over a wall or hard object where the normal velocity is 0 at the interface.

Theorem 2.11:

The single source representation (Equation7) for the half-space Ωh+ for a density φH(-1/2)(Γh) yields the integral representation of the power operator in (Equation15)(38) Pshφ(x):=18πρcΓhφ(y)j0k|x-y|+hj0k|x-y|dS(y)(38)

Proof The proof of this theorem is found in [Citation11].

Theorem 2.12:

The double source representation (Equation8) for the half-space Ωh+ for a density φH(1/2)(Γh) yields the integral representation of the power operator in (Equation15)(39) Pdhφ(x):=18πρcΓφ(y)2j0(k|x-y|)ν(x)ν(y)+h2j0(k|x-y|)ν(x)ν(y)dS(y)(39)

Proof We proceed as Theorems 2.7 and 2.8, whereΥdh(x,y)=Ω0141iρωΦh(z,x)ν(z)ν(x)Φ(z,y)ν(y)¯+1iρωΦh(z,y)ν(z)ν(y)¯Φ(z,x)ν(x)dS(z).

for any domain Ω0,hR+3 that contains Ωh and have connected Ω0,h+. Assume that Ω0 is a ball Br for some r>0. Since Br contains Ωh then r=|z|>|x| and r=|z|>|y| then we have the Half-space spherical harmonic representations (see [Citation11])Φh(z,y)ν(y)=ik2n=0m=-nnν(y)·y|y|jn(k|y|)Ynm(y^)¯+hYnm(y^)¯hn(k|z|)Ynm(z^)Φh(z,x)ν(z)ν(x)=ik3n=0m=-nnν(x)·x|x|jn(k|x|)Ynm(x^)¯+hYnm(x^)¯hn(k|z|)Ynm(z^)

This yields the representationΥsh(x,y)=k38ρωn=0ν(x)·x|x|ν(y)·y|y|jn(k|x|)jn(k|y|)×m=-nnYnm(x^)¯+hYnm(x^)¯Ynm(y^)+hYnm(y^)+O1r.

and the fact that r>0 can be arbitrarily large we conclude formula (Equation39).

Similarly we can prove the theorem.

Theorem 2.13:

The representation (Equation9) for a density φH(1/2)(Γ) and any η>0, yields the integral representation of the power operator in (Equation15)(40) Pcφ(x):=Pdhφ(x)+η2Pshφ(x).(40)

3. Numerical methodology

The numerical methodology will require the discretization of the different surface integral equations introduced in the previous sections. We choose the BEM to produce these discretization, since it is the classical accurate numerical methodology in the area of acoustics (see [Citation15,Citation16,Citation26]).

Assume that the pressure measurements are given by pmCm×1 over m points over the measurement surface Γ0 and define as pv,vvCn×1 the pressure and normal velocity over n points in the vibrating surface Γ. Similarly we define φCn×1 the density φ in (Equation6), (Equation9) over Γ. Moreover Γ is decomposed into triangular elements with three nodes. In this paper (as recommended in [Citation16]), iso-parametric linear functions are selected for interpolating the integral quantity φ. Denote as S,KCm×n the BEM discretization of the single layer operator S and double layer operator K in (Equation3) for xΓ0. In addition define as Ps,PdCn×n the discretizations of the power operators Ps,Pd in (Equation32), (Equation33).

An evenly distribution of points on the vibrating surface Γ can be used to produce a triangular surface element decomposition. Basic BEM calculations over the resultant surface element decomposition produces integration weights wi (see [Citation27]), i=1,,N such thatinwi=Area(Γ),wi>0.

The power is approximated directly from the exact pressure pv and velocity vv using(41) Πk12ReW1/2vvW1/2pv,(41)

where W=diag(w1,,wn).

Since Ps, Pd and η>0Pc=Pd+iηPs

are the discretization of positive definite operators, then we can compute the corresponding numerical eigenvalue decomposition(42) Ps=i=1nλi(s)ui(s)ui(s),Pd=i=1nλi(s)ui(d)ui(d),Pc=i=1nλi(s)ui(c)ui(c),(42)

where ui(s),ui(d),ui(c), i=1,,n are sets of orthonormal vectors. Here λi(s),λi(d),λi(c) denote the positive decreasing sequence of eigenvalues. The numerical identification of the supersonic field from pressure measurements in Γ0 for the single layer representation (Equation7) is reduced to the solution of(43) Sφs=pm,φsspanu1(s),,un(s),(43)

for the double layer representation (Equation8) is reduced to the solution of(44) Kφd=pm,φdspanu1(d),,un(d),(44)

and finally for the combined representation (Equation9)(45) K-iηSφc=pm,φcspanu1(c),,un(c).(45)

The resultant solutions of (Equation43)–(Equation45) are given byφs=i=1nCi(s)ui(s),φd=i=1nCi(d)ui(d),φc=i=1nCi(c)ui(c)

then the supersonic density and corresponding non-negative intensity as(46) ϕs=i=1nλi(s)Ciui,ϕd=i=1nλi(d)Ciui,ϕc=i=1nλi(c)Ciui,Isss=|ϕs|2,Idss=|ϕd|2,Icss=|ϕc|2.(46)

For the following numerical experiments we choose to validate the proposed SSI methodology using smooth surfaces Γ and Γ0. The surfaces of Γ and Γ0 correspond to the surface of spheres centered at the origin, respectively with radius of 1 and 1.05 m. The spherical surfaces are decomposed into 4990 points over 9976 triangles (as shown in Figure 3a of [Citation11]). At Γ, the maximum diameter between edges of the triangles is 5 cm and in Γ0 we keep an identical point distribution.

In all numerical experiments, the measured pressure at a point xΓ0 is generated by the sum of the a combination of monopoles distributed over an interior spherical surface. The analytical formula used to compute the field for each monopole is given by (Equation5). The column vector pm contains the exact generated pressure p in Γ0 added by the vector e with Gaussian entries and 40 dB signal-to-noise ratio to simulate measurement errors, i.e.pm=p+e,20lnpm-p2p2=-40.

Figure 3. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Dirichlet eigenvalue frequency 171.5 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 3. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Dirichlet eigenvalue frequency 171.5 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 4. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Dirichlet eigenvalue frequency 446.69 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 4. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Dirichlet eigenvalue frequency 446.69 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

3.1. Dirichlet eigenvalues

We use the conditions of air, with sound speed c=343ms-1 and density ρ=1.21Kgm-3. The 12 monopoles, used to generate the data, are distributed over a sphere of radius 0.9 m with (θ,ϕ) locations shown in Figure (a). Between the monopoles, the minimal arc-length distance over the ϕ directions is 60 cm and over the θ direction is 40 cm. In addition there is one monopole located at the north pole and one at the south pole.

Table 1. Results from non-negative intensity calculation for Dirichlet eigenvalues.

We apply the proposed numerical supersonic decompositions in (Equation46) for frequencies that correspond to k=3.1415,4.4934,5.7634,6.9879,8.1825 (Dirichlet eigenvalues). As stated in Corollary 2.9 this means that the operator Ps contains zero eigenvalues and this potentially could affect the accuracy of the intensity Isss. Table shows the total power Π at Γ numerically calculated from the exact pressure pv and normal velocity vv as in (Equation41). We denote as Πs the power that results from the proposed non-negative intensity Isss, and similarly Πd, Πc are the resultant power from the non-negative intensity Idss, Icss. The parenthesis in Table show the corresponding relative error between the non-negative intensity and exact power. Notice as expected the non-negative intensity Isss can underestimate the exact power for some of these problematic frequencies.

Figure (a) shows the exact intensity and Figure (b)–(d) shows the resultant non-negative intensities Isss, Idss, Icss over the spherical plane θ, ϕ at 171.5 Hz, and Figure shows these intensities at 446.69 Hz. The resolution of the proposed non-negative intensity images corresponds to half-wavelength resolution (1 and 38 cm respectively). Both the non-negative intensities Idss and Icss estimates the correct power but fail to localize sources in 446.69 Hz. Interestingly the images in Figures (b) and (b) shows that the intensity Isss, even that fails to estimate the correct power, tends to localize the noise sources.

3.2. Neumann eigenvalues

We utilize the same fluid conditions of the previous subsection. We produce data using only 10 monopoles, distributed over a sphere of radius 0.9 m with (θ,ϕ) locations shown in Figure (a). The spacing of monopoles are similar to the previous subsection, without the north pole and one at the south pole positions. We apply the proposed numerical supersonic decomposition in (Equation46) for frequencies that correspond to k=2.0815,3.3420,4.4934,4.5140,5.6467 (Neumann eigenvalues). As stated in Corollary 2.9 this means that the operator Pd contains zero eigenvalues and this potentially could affect the accuracy of the intensity Idss. As in Tables and shows the exact power Π and Πs, Πd, Πc are the resultant power from the non-negative intensity Isss, Idss, Icss. Notice that the non-negative intensity Idss from the double layer representation in (Equation7), can underestimate the exact power for some of these frequencies.

Table 2. Results from non-negative intensity calculation for Neumann eigenvalues.

Figure 5. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Neumann eigenvalue frequency 245.3 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 5. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Neumann eigenvalue frequency 245.3 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 6. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Neumann eigenvalue frequency 308.25 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 6. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the Neumann eigenvalue frequency 308.25 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 7. Plot of the multi-frequency acoustical response that results from the proposed point forces. The lower part of the pictures shows the spherical plane θ, ϕ view of the acoustical pressure measurement hologram at the surface Γ0 for different frequencies.

Figure 7. Plot of the multi-frequency acoustical response that results from the proposed point forces. The lower part of the pictures shows the spherical plane θ, ϕ view of the acoustical pressure measurement hologram at the surface Γ0 for different frequencies.

Figure (a) shows the exact intensity and Figure (b)–(d) resultant non-negative intensities Isss, Idss, Icss over the spherical plane θ, ϕ at 245.3 Hz, and Figure shows these intensities at 308.25 Hz. The resolution of the proposed non-negative intensity images corresponds to half-wavelength resolution (70 and 56 cm respectively). The non-negative intensity Isss estimates the correct power and correctly localizes sources (as we found in the numerical experiments of [Citation11]). The intensity images of Idss and Icss have a problem localizing the noise sources.

4. Physical experiments

To simulate realistic conditions of a complex structural vibration experiment, we utilize the spherical shell model described in Appendix 1. The resultant field produced by this model have been proven to be realistic for scattering experiments [Citation28,Citation29]. We assume the conditions of underwater thin hollow spherical steel shell, i.e. exterior water medium, interior air medium with steel shell. The dimensions under this conditions are given by the parameters (see Appendix 1) r1=1 m, r2=0.95 m, c1=1481ms-1, ρ1=998.2Kgm-3, λ2=9.695×1010Nm-2, μ2=7.617×1010Nm-2, ρ2=7700Kgm-3 and c3=343ms-1, ρ3=1.225Kgm-3. We set 6 point forces to produce the radiating field. The point forces are located at the north and south pole, and around 4 locations in the (ϕ,θ) plane shown in Figure (a). Two point forces are separated over the azymuth direction by 60 cm and two are separated over 1 m over the elevation direction.

Figure 8. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the resonant frequency 1009 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 8. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the resonant frequency 1009 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 9. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the resonant frequency 1346 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 9. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the resonant frequency 1346 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 10. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the non-resonant frequency 1080 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 10. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the non-resonant frequency 1080 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 11. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the non-resonant frequency 2160 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

Figure 11. Elastic shell data. Image of the non-negative intensity using the power operator over the spherical plane θ, ϕ at the non-resonant frequency 2160 Hz. (a) Exact intensity, non-negative intensity, (b) Isss, (c) Idss, and (d) Icss.

We utilize the same point distribution in the sphere surfaces Γ, Γ0 that we use in the Sections 3.1 and 3.2. This distribution allow us to apply the proposed numerical non-negative intensity methodology up to 4 kHz without violating the wavelength sampling. In Figure we show a typical multi-frequency structural acoustic analysis, where we compute the total pressure response p12(Γ) at each frequency. This allow the noise engineer to identify the resultant acoustic ‘resonances’ which are the frequencies were the structure produces the maximum vibration (peaks of the total pressure response). For our analysis we will process the non-negative intensity reconstructions at the resonance frequencies and analyze two non-resonant frequencies and a frequency that corresponds to the Dirichlet eigenvalue. The lower part of Figure shows the resultant pressure hologram at the surface Γ0 for four frequencies. Notice that is hard to identify the location of the point forces just by visual inspection.

Table 3. Results from proposed non-negative intensity calculation for the elastic sphere experiment.

In Table we show the power Π numerically calculated from the exact pressure pv and normal velocity vv as in (Equation41), and the corresponding power Πs,Πd,Πc that results from the proposed non-negative intensities Isss,Idss, Icss. The parenthesis in Table show the corresponding relative error between the non-negative intensity power and exact total power. An important result from this table is the fact that all non-negative intensity methods accurately estimate the exact power at all frequencies. Is interesting to point out that even at a problematic frequency 740.5 Hz, like wavenumber k=π that correspond to a Dirichlet eigenvalue, Isss correctly estimates the power.

Figures and shows the resultant non-negative intensities Isss, Idss, Icss over the spherical plane θ, ϕ at the resonant frequencies 1009 and 1346 Hz. All the non-negative intensities Isss, Idss and Icss estimates the correct power but fail to localize sources at both frequencies. We argue that at resonant frequencies the complete sphere structure is vibrating, so a localization of the sources cannot estimate the total power.

Figures and shows the resultant non-negative intensities Isss, Idss, Icss over the spherical plane θ, ϕ at the non-resonant frequencies 1080 and 2160 Hz. As the previous results, all the non-negative intensities estimates the correct power. But at these frequencies the intensity Isss localize the noise sources better than Idss, Icss.

5. Conclusion

Sections 2 and 3 extended the theoretical results of [Citation10,Citation11]. We have shown explicit non-negative intensity formulae from power operators that corresponds to different layer representations. The resultant intensity images Isss, Idss, Icss from numerically generated data demonstrate that the proposed non-negative intensity can be effectively used to estimate the total power in realistic situations. In addition, the non-negative intensity Isss localizes better the radiation regions for arbitrary surfaces.

Although not discussed in this paper, we can combine all of the previous approaches to identify correctly the radiation regions of the structure. The non-negative intensity Isss provides localized information of the sources, while Icss can effectively alert the analyst of possible resonant behavior. Also there are still questions about the computation of the non-negative intensity for lower frequencies in which the acoustic half-wavelength is larger than the vibrator surface. Here it is possible to consider the inverse source for single frequencies which has been extensively studied by other authors (see [Citation30Citation32]).

Additional information

Funding

This work was supported by the Office of Naval Research.

Notes

No potential conflict of interest was reported by the author.

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Appendix 1

Spherical shell

We describe the harmonic model of a spherical elastic shell excited by a point force. The analytical formulae of the scattering response correspond to a classical acoustical problem that can be found in [Citation33Citation35]. It is also important to mention that this formulae has been successfully validated with experimental data [Citation28,Citation29]. The numerical model that we will describe in this section is a generalization of previous works and includes the model of the interaction between a point force and the elastic medium suggested in [Citation1].

Let Br be a ball centered at the origin with radius r>0, and the corresponding boundary is denoted as Γr. We define the shell structure using radius r1>r2>0 as in Figure . Outside Br1 we have that the acoustic pressure p1 solves (Equation1) and the harmonic representation is given by(A1) p1(x)=n=0m=-nnAnmhn(k1|x|)Ynmx^,(A1)

where hn is the spherical Hankel function of the first kind and k1=ω/c1. At the shell Br1\Br2 we have that the displacements u2 solve the isotropic elastic medium equation(λ2+2μ2)graddivu-μ2curlcurlu2+ω2ρ2u2=0

where λ2,μ2 are the Lame’s elastic parameters and ρ2 the density of the elastic medium. The harmonic representation is given by(A2) u2(x)=gradxφ2(x)+curlxxϕ2r(x)+curlxxϕ2t(x)(A2)

where(A3) φ2(x)=n=0m=-nnBnmjn(kl1|x|)+Cnmyn(kl1|x|)Ynmx^ϕ2r(x)=n=0m=-nnDnmjn(ks1|x|)+Enmyn(ks1|x|)Ynmx^ϕ2t(x)=n=0m=-nnFnmjn(ks1|x|)+Gnmyn(ks1|x|)Ynmx^(A3)

Here jn, yn are respectively the spherical bessel and Neumann functions, and kl1=ωρ2/(λ2+2μ2), ks1=ωρ2/μ2. At the fluid inside Br2 we have(A4) p3(x)=p3p(x)+p3s(x)(A4)

where p3p is the pressure corresponding to a point force and p3s the resultant scattered wave(A5) p3p(x)=n=0m=-nnFpYnmy^¯r22Ynmx^p3s(x)=n=0m=-nnHnmjn(k3|x|)Ynmx^(A5)

Here k3=ω/c3 and Fp represents the force (N).

Figure A1. Elastic Shell model. Interior and Exterior domain are homogeneous acoustic mediums and shell contains elastic properties.

Figure A1. Elastic Shell model. Interior and Exterior domain are homogeneous acoustic mediums and shell contains elastic properties.

The interaction between acoustic pressure p1 in a fluid and the displacement u2 in an elastic medium is given by the boundary conditions at Γr1(A6) u2·ν=-1ρω2νp1,Tu2·ν=p,Tu2×ν=0(A6)

whereTu:=λνdivu+2μνu+μν×curlu.

At Γr2 we encounter the boundary condition(A7) u2·ν=0,Tu2·ν=Fpδ(y),Tu2×ν=0(A7)

that models the application of a point force in yΓr2.

Using boundary conditions (EquationA6) in Γr1 and (EquationA7) in Γr2 we obtain the matrix systems(A8) d11d12d13d14d150d21d22d23d24d2500d32d33d34d3500d42d43d44d45d460d52d53d54d55d560d62d63d64d650AnmBnmCnmFnmGnmHnm=b1b2b3b4b5b6(A8)

and(A9) f11f12f21f22DnmEnm=00(A9)

whered11=1ρ1ω2k1r1hn(k1r1),d12=kl1r1jn(kl1r1),d13=kl1r1yn(kl1r1),d14=n(n+1)jn(ks1r1),d15=n(n+1)yn(ks1r1),d21=-hn(k1r1),d22=kl122μ2jn(kl1r1)-λ2jn(kl1r1),d23=kl122μ2yn(kl1r1)-λ2yn(kl1r1),d24=2μ2n(n+1)r12r1ks1jn(ks1r1)-jn(ks1r1),d25=2μ2n(n+1)r12r1ks1yn(ks1r1)-yn(ks1r1),d32=2kl1r1jn(kl1r1)-jn(kl1r1),d33=2kl1r1yn(kl1r1)-yn(kl1r1),d34=ks12r12jn(ks1r1)+(n+2)(n-1)jn(ks1r1),d35=ks12r12yn(ks1r1)+(n+2)(n-1)yn(ks1r1),d42=kl1R2jn(kl1r2),d43=kl1r2yn(kl1r2),d44=n(n+1)jn(ks1r2),d45=n(n+1)yn(ks1r2,d46=1ρ3ω2k3r2jn(k3r2),d52=kl122μ2jn(kl1r2)-λ2jn(kl1r2),d53=kl122μ2yn(kl1r2)-λ2yn(kl1r2),d54=2μ2n(n+1)r22r2ks1jn(ks1r2)-jn(ks1r2),d55=2μ2n(n+1)r22r2ks1yn(ks1r2)-yn(ks1r2),d56=-jn(k3r2),d62=2kl1r2jn(kl1r2)-jn(kl1r2),d63=2kl1r2yn(kl1r2)-yn(kl1r2),d64=ks12r22jn(ks1r2)+(n+2)(n-1)jn(ks1r2),d65=ks12r22yn(ks1r2)+(n+2)(n-1)yn(ks1r2),f11=ks1r1jn(ks1r1)-jn(ks1r1),f12=ks1R1yn(ks1r1)-yn(ks1r1),f21=ks1r2jn(ks1r2)-jn(ks1r2),f22=ks1R2yn(ks1r2)-yn(ks1r2),

andb1=b2=b3=b4=b6=0,b5=FpYnmy^¯r22.

The resultant coefficients of the scattering wave (EquationA1) are found from the solution of the matrix Equation (EquationA8) for each nm. This normally is done numerically, but a few analytical approximations can be found in [Citation33].

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