Effective wave numbers for media sustaining the propagation of three types of bulk waves and hosting a random configuration of scatterers F. Luppéa , J.-M. Conoirb and A. N. Norrisc a LOMC-GOA, Université du Havre, place R. Schuman, 76610 Le Havre, France, Metropolitan b CNRS, Institut Jean Le Rond d’Alembert - UMR CNRS 7190, Université Pierre et Marie Curie - 4 place Jussieu, 75005 Paris, France c Rutgers University, Mechanical and Aerospace Engineering, Piscataway, NJ 08854, USA francine.luppe@univ-lehavre.fr Wave propagation through an isotropic host medium containing a large number of randomly and uniformly located scatterers is considered at low frequency and for low concentrations of spheres, and the dispersion relation of the coherent waves is obtained. The same problem had been addressed by Lloyd and Berry for spheres in an ideal fluid, and more recently by Linton and Martin for cylinders in an ideal fluid, and by Conoir and Norris for cylinders in an elastic solid. Here, the dispersion relation is derived in the case of spheres, and extended to that of cylinders, from the comparison of the 3d and 2d cases in an elastic solid. The host medium considered may support the propagation of P different types of bulk waves, as for example a thermo-viscoelastic medium or a poro-elastic medium (P=3). As in the previous works mentioned above, the hole correction of Fikioris and Waterman is taken into account, along with the quasi-crystalline approximation. The method follows exactly that used by Conoir and Norris. 1 Introduction This paper summarizes some of the results obtained in Refs.[1,2] on the propagation of coherent waves in homogeneous media that contain distributions of either spherical (d=3) or cylindrical (d=2) inhomogeneities acting as scatterers. It is focused on the low frequency and low concentration approximations of the dispersion equation of the coherent wave associated with the “fastest wave” in the host medium (more precisely, the wave which has the smallest modulus of all complex wave numbers). In a porovisco-elastic medium obeying Biot’s theory, for example, that would be the fast longitudinal wave. The method used to obtain the equations that govern the coherent fields follows that of Fikioris and Waterman’s paper [2]. A harmonic plane wave propagating in the host medium is supposed to be normally incident upon some (d ) semi-infinite region x > 0 hosting a uniform concentration of scatterers. In case of spherical scatterers, x(3) will be equal to z, while in case of infinitely long cylinders, x(2) will be equal to x, and the axis of the cylinders will be parallel to the z axis, so that the problem will be of dimension d=2. This harmonic plane wave gives rise to a multiple scattering process and to scattered waves of different polarization types denoted by a natural number p. When averaged over all possible locations of the scatterers, the total field of a given type p represents the coherent wave of type p. For a low enough concentration of scatterers, the coherent waves are supposed to be plane (d ) waves that propagate in the same direction x as the original incident plane wave. In the following, we suppose that the host medium supports the propagation of P different types of waves (P=1 in an ideal fluid, P=2 in an elastic solid, P=3 in a thermovisco-elastic medium or a poroelastic solid); they are numbered from p=1 to p=P, and their complex wave numbers at the given angular frequency ω are kp, with ∀p ≠ 1, k1 < k p , (1) so that the coherent we shall focus on in the last section corresponds to p=1. We shall also suppose, with no loss of generality but in order to simplify the d=3 dimensional ( p) problem, that the original incident plane wave, ϕinc , is also of type p =1, i.e. a longitudinal wave. An e-iωt time dependence of all fields, while supposed, will be omitted everywhere for the sake of brevity : ( ) ϕinc = δ p1e p d ik p x( ) , k p = k p ′ + ik p ′′ , k p ′ > 0, k p ′′ ≥ 0 . (2) 2 Coherent fields in the framework of the Fikioris and Waterman theory The waves are described by scalar displacement potentials. In the d=3 dimensional problem, these are the Debye potentials [4] of the longitudinal and shear waves : the Debye potentials of transverse waves are not taken into account for symmetry reasons linked to the longitudinal nature of the incident wave of Eq.(2), as explained in Ref.[2]. In the d=2 dimensional case, the scalar potentials are the displacement potential of the longitudinal waves and the z-component [5] of the vector potential of the shear waves. The total potential associated with a wave of type p is due to the incident wave, if of the same type, and to all the scattered waves of type p, so that, considering a given number N of scatterers, N (1) ϕ( p) r = δ p1ϕinc + ∑ ϕS( p) r ; rk . () k =1 ( p) Here, as in Ref.[1], ϕS ( ) (3) (r; r ) represents the wave (of k type p) that is scattered by a scatterer centered at rk and ( p) observed at r . Letting ϕE (r; r ) denote the field (of type k p) that is exciting a scatterer centered at rk and observed at r , the following equation defines the linear scattering (qp) rk of the scatterers operators T ( ) P ϕS( p) r ; rk = ∑ T (qp) rk ϕ(Eq) r ; rk . ( ) q=1 ( ) ( ) (4) The exciting field acting on the k-th scatterer is the sum of the incident field and the scattered waves from all the other scatterers: P N (1) ϕ(Ep) r ; rk = δ p1ϕinc r + ∑∑ T (qp) rj ϕEq r ; rj ,(5) ( ) () q=1 j =1 j≠k ( ) ( ) and the average exciting field on the 1st scatterer (supposed fixed), within the quasi-crystalline approximation, is given by p (1) ϕ(E ) r ; r1 = δ p1ϕinc r + ( ) ∫ () d rj n rj , r1 P with , (6) ( ) ∑ T (r ) ϕ (r; r ) (qp) ( q) j E N ( p) (ξk ) = ξk bj ′ (ξk b) h(1) ( k pb) − k pbj (ξk b) h(1)′ ( k pb) j q =1 with the integration performed over the whole region that hosts the centers of the scatterers and n rj , r1 , the conditional number density of scatterers at rj if one is known to be at r1 , given by the “hole correction” [3] : ( ) n0 for r − rj > b n r , rj = with b>2a. 0 otherwise (7) The effective potentials are expressed as infinite series that respect the symmetries of both the incident wave and the scatterers (see section II.B in Ref.[2]), d = 3, +∞ ϕE( p) r ; rj = ∑ An( p) rj jn ( k p ρ j ) Pn cos θ ρ j d = 2, ϕEp r ; rj = ( ) +∞ ∑ n=−∞ ( ( ) n =0 ( ) ( ) ( )) d = 2, An( p) P An( )e pk n j . (9) iξ k X j pk P +∞ +∞ 4n0 πb ξk2 − k p2 (qp) ν q =1 ν =0 =0 pk ) = 2πn0 2 ξk − K p2 q +∞ +∞ ∑ i J (k r ) e n n , (13) inθ q n=−∞ qp ) , +∞ ϕ(qp) = ∑ i n (2n + 1)Tn(qp)hn(1) ( k p r ) Pn (cos θ ) n=0 d = 2, +∞ ∑ i T( n n qp) , (14) H n(1) ( k p r ) einθ by a single scatterer centered at x=y=z=0. 3 Low frequency and low concentration approximation for all coherent wave dispersion equations The low frequency approximation corresponds to small values of k pb , whatever that of p. In the low concentration approximation, it is assumed that ξ p and kp are close enough for the expansion of ξ p2 − k p2 in terms of powers of ∀p ∈ {1, 2,3} , ∑∑∑ (−1) (2ν + 1)T d = 2, An( scattering of a type q incident wave ϕi( ) , n0 to be accurate enough at order 2: ∀p ∈ {1, 2,...P} , ∀k ∈ {1, 2,...P} = the modal coefficient associated with the n=−∞ Determination of the system of equations the An( ) amplitudes obey involves the decomposition of the incident plane wave, Eq.(2), into either spherical or cylindrical functions, the writing of the wave scattered by one scatterer as a sum of waves incident on the other scatterers via an addition theorem [6,7], and leads (see Refs.[1,2] for details), for identical scatterers, to pk ) qp ) ϕ(qp) = k =1 d = 3, An( and Tν( into a type p wave ϕ( in both cases, k =1 =0 d = 3, P iξ X rj = i n ( 2n + 1) ∑ An( pk )e k j (r ) = i ∑ Pn ( cos θ ) Pν ( cos θ ) = ∑ G ( 0,ν | 0, n | ) P ( cos θ ) , (12) ,(8) (d ) ( ) and the Gaunt coefficients G (0, ν | 0, n | ) defined from d = 2, ϕi = Descartes laws of refraction, i.e. they propagate in the x direction : d = 3, An 1 (11) ( q) and we assume the coherent waves obey the Snell- ( p) 1 n =0 ( ) with ρ j = r − rj and θ ρ j = Arg ρ j N mp (ξk ) = ξk bJ m′ (ξk b) H m( ) ( k pb) − K pbJ m (ξk b) H m( )′ ( k pb) d = 3, ϕi(q) = ∑ i n (2n + 1) jn ( kqr ) Pn (cos θ ) inθ(ρ j ) A rj J n ( K p ρ j ) e p n d = 2, +∞ ( ) ( ) d = 3, P (qk ) ( p) Aν N (ξk )G (0, ν | 0, n | ), +∞ ∑ ∑ T( q =1 m=−∞ qp) m Am( ) N mp−n (ξk ) qk (10) ⎛ ⎟⎞ P ⎜⎜ (d ) .(15) d) ⎟ ( ξ − k = d1 p n0 + ⎜⎜d 2 p + ∑ d 2 pq ⎟⎟⎟ n02 + O (n03 ) ⎜⎜ ⎟⎟ q=1 ⎝⎜ ⎠ q≠ p 2 p 2 p (d ) Equations.(11) are infinite linear and homogeneous pk systems of equations for the unknown amplitudes An( ) ; setting their determinants to zero provides the dispersion equations of the p-type coherent wave (once again, see Ref.[2] for details), which, under both assumptions of low concentration and low frequency, leads to (3) d1 p = −4iπk 3 p +∞ ∑(2n +1)T ( pp) n , Eq.(14) at a large distance r from a single scatterer centered at x=y=z=0 : d = 3, ϕ( pq) (r , θ ) (16) n=0 +∞ +∞ +∞ ϕ n=0 m=0 ν =0 ( pq ) (r , θ ) ( pp) ( pp) (2m +1)(2n +1)Tn Tm νG (0, m | 0, n | ν ) d 2(3pq) = −16π 2 k 9p +∞ +∞ +∞ (17) ∑∑∑ kq (k p2 − kq2 ) n=0 m=0 ν =0 ikq r f pq(3) (θ ) r kq . −iπ / 4 e e ( 2) 2 f pq (θ ) π kq1/ 2 ikq r r (r →+∞) (20) (2) with, in case of a circular cylinder, f pq an even function of θ if p and q are associated both to either longitudinal or shear waves, and an odd function if only one is associated with a longitudinal (or shear) wave. ν ⎛ ⎞ ⎜⎜ ⎟ G (0, m | 0, n | ν ) ⎜⎝ kq ⎟⎠ (qp) ( pq) ⎜ k p ⎟ ⎟ (2m +1)(2n +1)Tn Tm e d = 2, d 2( p) = −8π 2 k p6 ∑∑∑ 3 (r →+∞) −i (d ) (d ) (2) While d1 p , d 2 p , and d 2 pq have all been written [810,1] in terms of the far field form functions defined by (3) Eq.(20), we have not managed to do the same for d 2 pq , for the spherical case, and to d1(2p) = −4ik p2 +∞ ∑ T( pp) n , (18) unless p=1 and obeys Eq.(1) ; this is the reason why we focus now on the coherent wave that is associated with the fastest longitudinal wave p=1. We found indeed [2] : n=−∞ d 2( p) = −8k p4 2 +∞ +∞ ∑ ∑ m − nTn( )Tm( pp π f1(q ) (θ ) f q(1 ) (θ ) 8π 2 sin θd θ ,(21) d 21q = k p ∫0 (k p2 + kq2 − 2k p kq cos θ )3/ 2 pp) n=−∞ m=−∞ ⎛ k ⎞⎟ ⎜⎜ p ⎟ d 2 pq = −16 2 ⎟ 2 ∑ ∑ ⎜ k p − kq n=−∞ m=−∞ ⎜⎝ kq ⎠⎟ k p6 (2) +∞ +∞ ,(19) m−n (qp) ( pq) Tn Tm (2) 2 while the equivalent term in the d=2 case was [1] : π ( ) ( ) ( ) ( ) 8 f1q (θ ) f q1 (−θ ) + f q1 (θ ) f1q (−θ ) d 21q = ∫ dθ . π 0 k12 + kq2 − 2k1kq cos θ 2 (2) for the cylindrical case. (3) 2 (3) 2 2 2 (22) In both cases, the first order terms d1 p and d1 p , that involve no mode conversion, do not depend on the complexity of the host medium. The second order terms that exhibit as well no mode conversions had been given by Lloyd and Berry for spheres in an ideal fluid [8,9], and by Linton and Martin for cylinders [10,1]. The coupling term (2) for cylinders, d 2 pq ,was obtained by Conoir and Norris [1]. In Ref.[2], we used the matrix formalism developed by the latter to obtain its spherical counterpart. While Eqs.(15-19) are the most suitable for numerical computations, the dispersion equations are most often presented in terms of the far-field scattering functions of the scatterers. This is the object of next section. 4 Low frequency and low concentration approximation of the dispersion equation of the fastest coherent wave in terms of far-field scattering functions Equations.(20) define the far-field scattering functions (d ) f pq (θ ) from the expression of scattered fields as in Reducing the d=2 case to circular cylinders whose far field functions have the parity properties afore mentioned, and defining vectors k1 .kq = k1kq cos θ , and k1 = k1 X , kq such that k1q = k1 − kq , the dispersion equation of the coherent p=1 wave may be recast from Eqs.(15-22) into 2 n02 ξ12 (d ) n0 (d ) n0 δ δ = 1 + + + 11 21 k12 k1d k12 d k1d P ( ) δ21 q q =2 k1d ∑∫ d Ω( ) d d Ω (d ) , (23) (d ) with Ω the solid angle in the d-dimensional space. The first order terms and the uncoupling 2nd order terms are, as given in Refs.[8-10] (in Ref.[1], all integrals (2) corresponding to δ2 p should extend from 0 to π, instead of 2π) : δ11(3) = −4iπ f11(3) (0) δ11( ) = −4if11( ) (0) 2 2 , (24) π (3) δ21 = 4π 2 References 2 d 1 3 f11( ) (θ ) d θ ⎛ θ ⎞ dθ sin ⎜⎜ ⎟⎟⎟ ⎜⎝ 2 ⎠ ( ∫ 0 ) 2 2⎤ ⎡ +4π 2 ⎢ f11(3) (0) − f11(3) (π ) ⎥ , ⎢⎣ ⎥⎦ π ⎛θ ⎞ d 8 2 2 (2) f11( ) (θ ) d θ δ21 = ∫ cot ⎜⎜ ⎟⎟⎟ ⎜ ⎝ 2⎠ dθ π 0 ( ) ( ) ( (25) ) and the second order coupling terms may be written, from Eqs.(21-23), in a way that exhibits the similarities of the spherical and circular cylindrical cases : (3) δ21q = 4π (2) 21q δ f1(q3) (θ ) f q(13) (−θ ) k1d k1d ( 2) ( 2) 2 f1q (θ ) 2 f q1 (−θ ) =4 π k11/d 2 π k11/d 2 . (26) Looking back at Eqs.(24,16), one can only wonder if it is possible to write Eq.(25) in a similar way, such as () δ21 = 4π ∫ x (θ ) f11( ) (θ ) f11( )′ (θ ) dΩ ( ) 3 3 3 3 3 Ω( ) ( ) δ21 = 4 ∫ x (θ ) 2 2 Ω( ) 2 ( 2) 2 (2)′ 2 f11 (θ ) f11 (θ ) dΩ ( ) π π .(27) [1] J.M. Conoir, A.N. Norris, “Effective wavenumbers and reflection coefficients for an elastic medium containing random configurations of cylindrical scatterers”, Wave Motion 47, 183-197 (2010) [2] F. Luppé, J.M. Conoir, A.N. Norris, “Efective wave numbers for thermo-viscoelastic media containing random configurations of spherical scatterers”, J. Acoust. Soc. Am. 131(2), 1113-1120 (2012) [3] J.G. Fikioris and P.C. Waterman, “Multiple scattering of waves. II ‘hole corrections’ in the scalar case”, J. Math. Phys. 5(10), 1413-1420 (1964) [4] D. Brill, G. Gaunaurd, H. Überall, “Resonance theory of elastic shear-wave scattering from spherical fluid obstacles in solids”, J. Acoust. Soc. Am. 67(2), 414-424 (1980) [5] J.J. 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