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Proceedings. Mathematical, Physical, and Engineering Sciences logoLink to Proceedings. Mathematical, Physical, and Engineering Sciences
. 2016 Oct;472(2194):20160604. doi: 10.1098/rspa.2016.0604

Reciprocity, passivity and causality in Willis materials

Michael B Muhlestein 1,3, Caleb F Sieck 2,3, Andrea Alù 2, Michael R Haberman 1,3,
PMCID: PMC5095451  PMID: 27843410

Abstract

Materials that require coupling between the stress–strain and momentum–velocity constitutive relations were first proposed by Willis (Willis 1981 Wave Motion 3, 1–11. (doi:10.1016/0165-2125(81)90008-1)) and are now known as elastic materials of the Willis type, or simply Willis materials. As coupling between these two constitutive equations is a generalization of standard elastodynamic theory, restrictions on the physically admissible material properties for Willis materials should be similarly generalized. This paper derives restrictions imposed on the material properties of Willis materials when they are assumed to be reciprocal, passive and causal. Considerations of causality and low-order dispersion suggest an alternative formulation of the standard Willis equations. The alternative formulation provides improved insight into the subwavelength physical behaviour leading to Willis material properties and is amenable to time-domain analyses. Finally, the results initially obtained for a generally elastic material are specialized to the acoustic limit.

Keywords: elastic metamaterial, reciprocity, passivity, causality, Willis material

1. Introduction

Metamaterials are engineered composite materials that derive their interesting properties from hidden degrees of freedom [13]. One of the most interesting aspects of metamaterials is that their properties often surpass those of naturally occurring and man-made composite materials. For example, materials have been made with negative dynamic mass density [4], negative dynamic modulus [5] and negative phase speed [6]. Models of materials displaying generalized elastodynamic response which couples stress and momentum density to both strain and particle velocity have also been explored [710]. The latter class of materials is known as Willis materials, and their description requires the definition of an additional material parameter in the momentum and dynamic stress relationships [11]. In attempting to design materials with extreme properties, such as Willis materials, it is of critical importance to know the constraints placed on the material properties by fundamental physical laws. These constraints provide the scientist with an understanding of what material properties are physically meaningful and provides a deeper understanding of the material. It also gives both theoreticians and experimentalists a means to check that predicted or measured effective material properties do not violate underlying physical principles.

Restrictions on the range of material properties are derived from assumptions about the material itself. For example, standard elastic materials are assumed to be passive and causal. As passive elastic and acoustic metamaterials are composed of passive materials, they must also be passive and causal. Similarly, if all of the constituent materials are reciprocal, reciprocity must also be enforced [12]. The restrictions imposed on general Willis-type material properties due to passivity have been derived by Srivastava & Nemat-Nasser [9] and Srivastava [13]. The restrictions imposed by causality have been derived for general Willis materials [13], but the implications of these restrictions were not fully explored. The consequences of restrictions placed on Willis coupling parameters due to passivity, reciprocity and causality are the primary contribution of this work.

The purpose of this paper is to derive general restrictions on the material properties of a linear Willis material, which are described in §2. Reciprocity and passivity in Willis materials are discussed in §3 and then combined. Reciprocity is shown to impose a symmetry on the material properties corresponding to the major symmetries of the stiffness tensor. Passivity in a reciprocal material is shown to restrict the sign of the imaginary part of the density and stiffness tensors and the real part of the Willis coupling parameters. Section 4 investigates the requirements of causality in a local medium using arbitrary history functions. Considerations of low-order dispersion in the light of requirements imposed by causality suggest an alternative representation for Willis coupling which is more appropriate for time-domain analyses. Sections 5a,b present requirements on dispersion relations in two separate limiting cases, and §5c specializes in the restrictions on the material properties to the acoustic case for application to heterogeneous fluids. Section 6 then summarizes the work and discusses its relevance to the fields of acoustic and elastic metamaterials.

2. Constitutive equations and minor symmetries

A linear Willis material is a composite material which, when homogenized, requires the stress–strain and the momentum–velocity constitutive equations to be coupled. This non-intuitive coupling arises from both non-local effects and from material asymmetries [710]. Using standard index notation and assuming a time-harmonic motion (eiωt time convention), the generalized elastodynamic constitutive equations take the form [7,8,10]

σij=Cijkluk,l+Sijkvk 2.1a

and

μi=S~ijkuj,k+ρijvj, 2.1b

where σij is the Cauchy stress (hereafter called the stress), Cijkl is the stiffness tensor, ui,j is the displacement gradient, vi=u˙i is the particle velocity (hereafter called the velocity) with the over-dot denoting a time derivative, μi is the momentum density (hereafter called the momentum) and ρij is the mass density tensor. The third-order tensors Sijk and S~ijk represent a material property that couples the time-harmonic velocity to the stress and the time-harmonic strain to the momentum, respectively, and are therefore called coupling tensors. In general, all material properties are temporally and spatially dispersive, i.e. f(ω,k). Notice that equations (2.1) are written in the more general form using the displacement gradient rather than the strain [8].

Willis coupling encompasses all linear phenomena which generate stress from a net translation and linear momentum from local strain [11,14]. For example, in reciprocal media this coupling has been demonstrated to arise from asymmetry of a representative volume element (RVE) [10,14,15] and through non-local phenomena, such as lattice effects [16,17]. Willis coupling has also been demonstrated to arise in non-reciprocal media, although not described as such [18]. Willis coupling is mathematically analogous to bianisotropic materials in optics, and so chiral materials may also be considered a subset of general Willis materials [19]. For the sake of simplicity, the following derivation will assume that the Willis material is irrotational (so the displacement gradient ui,j may be replaced by the symmetric strain tensor εij) and only accounts for local interactions, unless explicitly stated otherwise.

For this set of assumptions, various symmetries of the material properties follow from standard elasticity. Assuming no external body forces, the stress tensor is symmetric [20], so the stiffness and the stress–velocity coupling tensor satisfy the symmetry conditions

Cijkl=Cjikl 2.2a

and

Sijk=Sjik. 2.2b

Likewise, as infinitesimal strains are symmetric by definition [20], the stiffness and the momentum–strain coupling tensor satisfy the symmetry conditions

Cijkl=Cijlk 2.3a

and

S~ijk=S~ikj. 2.3b

The conditions on the stiffness tensor in equations (2.2a) and (2.3a) are often called the minor symmetries of the stiffness tensor. Therefore, the restrictions placed on the coupling tensors in equations (2.2b) and (2.3b) will be referred to as the minor symmetries of the coupling tensors.

3. Reciprocity and passivity

Reciprocity is qualitatively described as being able to exchange a source and a receiver without changing the measured signal, and is a common characteristic of linear elastic and acoustic media [12]. A passive medium cannot generate energy. This is another way of stating that a passive material cannot amplify mechanical disturbances such as elastic waves as they propagate through it. Restrictions on the Willis material properties imposed by assuming that a medium reciprocal, passive or both passive and reciprocal will be derived in this section. It is noted that the constraints due to reciprocity and passivity have been derived elsewhere using an alternative approach [9].

(a). Reciprocity

As mentioned above, Willis material properties are a result of the homogenization of inhomogeneous elastic composites. As linear elastic materials are reciprocal, it follows that the emergent Willis material properties should also exhibit reciprocity [12]. The restrictions placed on the material properties of a linear Willis material, by assuming that they are reciprocal materials, are derived in this section. The present analysis differs from many analyses associated with reciprocity, in that we assume that the material is reciprocal to derive material symmetries, whereas previous work assumed material symmetries to derive reciprocity [12].

The dynamic equation for a time-harmonic linear elastic system may be written as the real part of

σij,jeiωt+fieiωt=μ˙ieiωt, 3.1

where f e−iωt is a time-harmonic body force density, σij,j represents the divergence of the stress field and the over-dot denotes a time derivative. Note that for time-harmonic systems μ˙iωμ. The solution to this equation is the displacement field ui. The common e−iωt may be neglected by noting that the stress, body force and momentum density can be complex-valued and represent the time-averaged fields.

Consider two elastodynamic source distributions in the same material, denoted A and B. These two source distributions are independent of each other, and arbitrary except that they satisfy the dynamic equations

σij,jA+fiA=μ˙iA 3.2a

and

σij,jB+fiB=μ˙iB. 3.2b

The solutions to equations (3.2a) and (3.2b) are the displacement fields uiA and uiB, respectively, which are not equal to each other in general. In order to determine the restrictions associated with reciprocity, one can employ the reaction principle [21]. For this case, the reaction principle simplifies to multiplying equation (3.2a) by the solution to equation (3.2b), uiB, and equation (3.2b) by the solution to equation (3.2a), uiA. The difference between these two relationships yields

(σij,jAuiBσij,jBuiA)+(fiAuiBfiBuiA)=(μ˙iAuiBμ˙iBuiA). 3.3

For convenience, define ΔFσij,jAuiBσij,jBuiA, ΔBfiAuiBfiBuiA, and ΔMμ˙iAuiBμ˙iBuiA, and so equation (3.3) becomes

ΔF+ΔB=ΔM. 3.4

Using the relations σij,jXuiY=[σijXuiY],jσijXui,jY=[σijXuiY],jσijXεijY, ΔF may be expanded as

ΔF=[σijAuiBσijBuiA],j(σijAεijBσijBεijA). 3.5

Further expanding the last term of equation (3.5) by assuming the medium in question is a Willis material with constitutive behaviour described by equations (2.1) yields

σijAεijBσijBεijA=CijklεijBεklACijklεijAεklB+SijkεijBvkASijkεijAvkB 3.6

for the second term on the left-hand side of equation (3.4). Similarly, if the medium in question is a Willis material, ΔM may also be expanded as

ΔM=S~ijkuiBε˙jkAS~ijkuiAε˙jkB+ρijuiBv˙jAρijuiAv˙jB=S~ijkviBεjkAS~ijkviAεjkB+ρijviBvjAρijviAvjB, 3.7

where the time-harmonicity in a linear time-invariant system has been used to move the time derivatives. Combining the results of equations (3.5)–(3.7) with equation (3.4), we may write

[σijAuiBσijBuiA],j+ΔB=(CijklεijBεklACijklεijAεklB)+(SijkεijBvkASijkεijAvkB)+(S~ijkviBεjkAS~ijkviAεjkB)+(ρijviBvjAρijviAvjB), 3.8

which may be simplified by exchanging dummy indexes to yield

[CijklCklij]εijBεklA+[S~ijkSjki](viBεjkAviAεjkB)+[ρijρji]viBvjA=[σijAuiBσijBuiA],j+ΔB.

The present analysis makes a point of departure here from previous analyses of reciprocity in generalized elastodynamics. Often, material symmetries are assumed and the reciprocity relations are derived. However, we will assume local reciprocity as derived by Achenbach [12] and then derive material symmetries. For a locally reciprocal, time-invariant material, it has been shown that ΔB=[σijAuiBσijBuiA],j, and we conclude

[CijklCklij]εijBεklA+[S~ijkSjki](viBεjkAviAεjkB)+[ρijρji]viBvjA=0. 3.9

As the choice of force source distributions was arbitrary, the strain and velocity fields must be considered independent fields. Therefore, the first and third terms in equation (3.9) must be individually equal to zero. Consequentially, the second term must also be zero, yielding

Cijkl=Cklij, 3.10a
ρij=ρji, 3.10b
andS~ijk=Sjki. 3.10c

The restriction placed on the stiffness tensor by elastodynamic reciprocity is given by equation (3.10a) and is called the major symmetry of the stiffness (alternatively obtained by considering an assumed strain-energy function [20]; this symmetry is usually used to derive reciprocity). Likewise, the symmetries required by reciprocity on the density tensor (usually treated as a trivially symmetric scalar) and the coupling tensors, equations (3.10b) and (3.10c), respectively, are also called major symmetries.

(b). Passivity

A passive mechanical medium is one that does not supply any mechanical energy. It can only respond to externally provided stimulus. This is expressed in terms of energy with the statement that net energy flux into a region of a passive material must be equal to or greater than zero. As with reciprocal media, any heterogeneous material constructed of passive materials must also be passive. This is true for standard elastic materials and generalized elastodynamic media like Willis materials. The restrictions imposed by passivity on Willis materials have also been derived by other authors (see [9,13]), but they are provided in this section for completeness. The present derivation will follow the approach of Banerjee [22].

The net energy flux per period into a finite-sized region Ω with boundary Γ is the real part of the complex power [23], while the imaginary part is known as the reactive power, which does not contribute to the energy transmitted to Ω. The complex power in the regions Ω, denoted by P, is given by

P=Γσijvinjdx+Ωfividx=Ω[σijvi,j+μ˙ivi]dx, 3.11

where ni is the unit outward normal, and the equation has been simplified using the divergence theorem and the dynamic equation given in equation (3.1). Using the Willis relations, equation (3.11) may be expanded as

P=Ω[Cijkluk,lvi,j+Sijkvkvi,j+S~ijkvj,kvi+ρijv˙jvi]dx. 3.12

Through the careful choice of boundary conditions, the velocity and strain in the region Ω may be imposed independently, assuming that Ω is small enough relative to a wavelength that no significant wave motion may occur within the domain. Therefore, one may set the particle velocity vi equal to zero to yield an inequality involving the stiffness, or one may set the strain equal to zero to yield an inequality involving the mass density, written respectively as

{Cijklvi,juk,l}=iω2(CijklCklij)εijεkl0 3.13a

and

{ρijviv˙j}=iω2(ρijρji)vivj0. 3.13b

For non-zero strain and non-zero velocity, passivity requires

{S~ijkvivj,k+Sijkvkvi,j}{Cijklvi,juk,l}{ρijviv˙j}. 3.14

(c). Reciprocal and passive media

If the medium is both reciprocal and passive, the major symmetries of the stiffness and density tensors can be exploited to simplify equations (3.13) to yield

Cijklεijεkl0 3.15a

and

ρijvivj0, 3.15b

where Y ′≡ℜ{Y } and Y ′′≡ℑ{Y }. In words, equations (3.15) mean that for a passive material and using the e−iωt time convention, the imaginary part of the stiffness tensor must be negative definite and the imaginary part of the density tensor must be positive definite. Equation (3.14) may also be simplified to give

{εij{Sijk}vk}εijCijklεkl+viρijvj. 3.16

In the light of equations (3.15), we find that the right-hand side of equation (3.16) must be either zero (the lossless case) or positive. In the important limiting case of a lossless material, we find

{Cijkl}={ρij}={Sijk}={S~ijk}=0. 3.17

These results were found using similar methods by Srivastava & Nemat-Nasser [9] and Srivastava [13].

The result that the coupling tensors must be purely imaginary in the lossless case is interesting, given the fact that complex coupling tensors have emerged from a derivation that only considers lossless media [10,15]. This is counter to the stiffness and density tensors which are purely real unless losses are present. For those properties, the imaginary component is non-zero because the material response lags the excitation in lossy media. On the other hand, the imaginary part of the coupling tensors have been associated with asymmetry at the inclusion scale [10,15], while the real part has been observed to be due to non-local coupling phenomena from ‘weak spatial dispersion effects associated with the finite phase velocity along the array’ [16]. This explains the apparent discrepancy between the present derivation, which does not account for such non-local phenomena, and the complex-valued predictions of the above-mentioned derivation which assumes a periodic lattice.

The bounds imposed by reciprocity may be derived for coupling tensors accounting also for non-local phenomena. As shown by Alù [16] and Sieck et al. [17], local coupling phenomena are accounted for by coupling tensors which are even in wavenumber which requires, for example, that Sijk(ω,k)=Sijk(ω,−k). On the other hand, first-order non-local coupling phenomena are accounted for by coupling tensors which are odd in wavenumber; for example, Sijk(ω,k)=−Sijk(ω,−k). In general, the coupling tensors may be a combination of even and odd components (labelled by superscripts), such that Sijk=Sijkeven+Sijkodd and S~ijk=S~ijkeven+S~ijkodd. While this distinction does not affect the results of the passivity derivation, including the odd component of coupling in the reciprocity analysis leads to the statement

S~ijkodd=Sjkiodd. 3.18

Combining equation (3.18) with equation (3.14) and assuming lossless media results in purely real values for Sijkodd and S~ijkodd. As mentioned in §2, all coupling tensors will be assumed to account only for local phenomena and will therefore be assumed to be even in wavenumber.

4. Causality

In general, the strain and velocity fields at a given time and location in a material depend upon the fields at other times (material memory) and locations (non-locality). By assuming that nothing in the future may affect the present state of the system (that is, the system is causal) one restricts the admissible functions that describe the material response [24,25]. Welters et al. showed that causality is guaranteed for linear and passive materials for electromagnetic wave propagation [26], which is similar to elastodynamic wave propagation in many respects. While causality is well known and often used in electromagnetism to provide restrictions on the spectral shape of material properties for special cases, the principle of causality has primarily been used in the fields of acoustics and elastodynamics for measurement purposes [2729]. Therefore, we will start our discussion of the effects of causality in a linear, local Willis material by deriving the Kramers–Krönig relations.

For the present analysis, it is assumed that only local effects are significant, and that all of the results will hold point-wise throughout the material. Despite the fact that lattice effects are known to be important in Willis materials [16], an analysis on the effects of non-local causality is beyond the scope of this work. For this case, a constitutive equation for a linear material relating a fields y^n(t) to the field x^(t) may then be written in the time-domain as a sum of convolutions [25]

x^(t)=n0(sA_n(s))y^n(ts)ds, 4.1

where A_n(s) are known as the history functions and are real valued. Note that A_n(s) and y^n(t) are not vectors, but a list of arbitrary tensors. As an example, y^1(t) could represent the strain field ε^ij(t) at a given material point as a function of time and A_1(s) would then represent the history function associated with the stiffness, C_ijkl(s) (note that it is not the stiffness). In that case, x^(t) would be the stress σ^ij(t) at the same material point as a function of time. The history functions are assumed to be smooth, except possibly at s=0, and are purely real. Further, the history functions are assumed to go to zero as s. For time-harmonic systems, we may write x^(t)={x(ω)eiωt} and y^n(t)={yn(ω)eiωt}, and the operator ℜ{⋅} and the time dependencies may be neglected by considering only time-averaged quantities. Then, integrating equations (4.1) by parts, multiplying the result by eiωt (the complex conjugate of our time convention e−iωt), and time averaging yields

x(ω)=n[A_n(0)iω0A_n(s)eiωsds]yn(ω). 4.2

One can then define the complex, frequency-dependent material properties, An, as

An(ω)A_n(0)+ω0A_n(s)sin(ωs)dsiω0A_n(s)cos(ωs)ds, 4.3

or simply An(ω)=An′(ω)+iAn′′(ω), where An(ω) and A′′n(ω) are the real and imaginary parts of An(ω), respectively, defined as

An(ω)=A_n(0)+ω0A_n(s)sin(ωs)ds 4.4a

and

An(ω)=ω0A_n(s)cos(ωs)ds. 4.4b

Equation (4.2) therefore simplifies to x(ω)=nAn(ω)yn(ω), and equation (4.3) may then be re-written in the following useful form:

An(ω)A_n(0)=(An(ω)A_n(0))+iAn(ω)=0A_n(t)iωeiωtdt. 4.5

The left-hand side of equation (4.5), AnA_n(0), is found to be analytic for any finite value of ω and at on the upper half of the complex-ω plane. Thus, in the limit ω, An(ω)A_n(0) and A′′n(ω)=0. Then, as An(ω)A_n(0)=An(ω)An() is analytic in the upper half complex-ω plane, Cauchy’s residue theorem allows one to express the material property, An, as

An(ω)An()=1πPAn(λ)λωdλ 4.6a

and

An(ω)=1πPAn(λ)An()λωdλ, 4.6b

where the P denotes the principal value of the integral. These relations are known as the Kramers–Krönig relations, and they explicitly relate A′′n(ω) to An(ω)A() via the Hilbert transform [30]. Note that any constant in the integrands will integrate to zero because the denominator is an odd function of ω. Finally, as An(ω) is even and A′′n(ω) is odd with respect to ω, the integrals in equations (4.6) may be reduced to only positive values of λ to give

An(ω)An()=2πP0λAn(λ)λ2ω2dλ 4.7a

and

An(ω)=2πP0ωAn(λ)λ2ω2dλ. 4.7b

Equations (4.7) must hold for any physically realizable system, and may be used to check that a predicted dispersion relation for an arbitrary material property is causal. For a linear Willis material, the constitutive equations (2.1) are therefore causal if the following relations between real and imaginary parts hold

Cijkl(ω)Cijkl()=2πP0λCijkl(λ)λ2ω2dλ,Cijkl(ω)=2πP0ωCijkl(λ)λ2ω2dλ, 4.8a
Sijk(ω)Sijk()=2πP0λSijk(λ)λ2ω2dλ,Sijk(ω)=2πP0ωSijk(λ)λ2ω2dλ, 4.8b
S~ijk(ω)S~ijk()=2πP0λS~ijk(λ)λ2ω2dλ,S~ijk(ω)=2πP0ωS~ijk(λ)λ2ω2dλ, 4.8c
andρij(ω)ρij()=2πP0λρij(λ)λ2ω2dλ,ρij(ω)=2πP0ωρij(λ)λ2ω2dλ. 4.8d

(a). An informative limiting case

Equations (4.8) provide explicit relationships between the real and imaginary parts of the dispersive properties of a causal Willis material. Unfortunately, the generality of these expressions does not lend itself to easy implementation in determining general theoretical restrictions imposed on Willis material properties by assuming causality. An important question, then, is: How can the Kramers–Krönig relations be used to learn more about Willis materials? Some answers to that question can be obtained by first acknowledging assumptions underlying the implementation of equations (4.8) and then investigating limiting cases. In order to use these relationships, one must first acknowledge the assumptions implicit in this formulation. The primary assumption relevant to this study is that the history functions that are valid and associated material properties describe a material that is well represented as a continuum. That is to say, one must assume that all small-scale physics underlying the dispersive nature of the medium are accurately represented by the history functions at every material point. For example, one does not need to explicitly consider molecular dynamics associated with relaxation in a viscoelastic medium to model the causal stress–strain response of the medium using a stiffness history function. Under the continuum hypothesis one must therefore assume that the upper limit of the integrals in equations (4.8) is only infinite in the sense that it is sufficiently high to not restrict the accuracy of the relationships between real and imaginary parts of the material property.

Beyond these basic assumptions, it is also important to note that it is rarely, if ever, possible to know the real or imaginary parts of any material property at all frequencies. Numerous authors have addressed this difficulty by limiting their analysis to certain frequency ranges where simplifying assumptions may be made such that knowledge of the material response outside of that range is unnecessary to provide accurate relations between the real and imaginary parts of a material property. Common examples include investigation of regions of low loss near poles [24] and limiting analysis to regions of weak dispersion [27]. These specific cases and their implications on dispersive Willis material properties will be discussed in more detail in §5a,b.

One specific limiting case of interest is that of a passive, reciprocal and lossless Willis material in the long wavelength limit. This case is of specific interest to the field of acoustic and elastic metamaterials, which focuses on effective properties of a medium that result from deeply subwavelength microstructure. In the long wavelength limit, one can evaluate the Kramer–Krönig relations if the upper limit of equations (4.8) is set to a frequency that is simultaneously much greater than the frequency of interest and well below the lowest microstructural resonance frequency. This interpretation of the integral limits is permissible because of the continuum approximation [31]. In this case, the material properties are local in time and space, and all losses are negligible. While the upper frequency limit described here is difficult, if not impossible, to define from a mathematical standpoint, the value of this approximation to aid in physical reasoning based on a causality argument will become clear in the following paragraphs. For this case, equation (3.17) provides the passivity requirement that the imaginary parts of the stiffness and mass density tensors are zero and the real parts of the coupling tensors are also zero at all frequencies considered in the Kramer–Krönig relations. The requirements of causality summarized in equations (4.8) then simplify to

Cijkl(ω)=Cijkl(),ρij(ω)=ρij(),{Sijk(ω)}={S~ijk(ω)}=0. 4.9

Thus, Willis coupling appears to be prohibited by causality in this limiting case. However, multiple investigators have predicted the existence of non-zero Willis coupling tensors in passive, lossless and reciprocal media in the very long wavelength limit. For example, Nemat-Nasser & Srivastava [15] and Norris et al. [10] used Bloch wave analyses to determine the effective coupling tensors for a one-dimensional elastic lattice, Sieck et al. provided estimates for the analogous one-dimensional acoustic system [17], and Milton calculated coupling tensors for a two-dimensional periodic lattice [32]. In all of these works, complex valued coupling tensors have been predicted in the low-frequency limit when all constituent materials of the microstructure were assumed to be lossless. One thus concludes that while equations (2.1) provide an accurate and insightful representation the behaviour of materials with asymmetric microstructure (i.e. they properly describe the motion of the system), they are not a universally causal representation. While a causal representation may not be necessary for frequency domain analyses, effective medium theory that does not provide causal effective properties may pose problems for time-domain analyses and to interpretation of experimental data [2729]. It is therefore important to investigate whether a causal representation can be found.

One common aspect of the studies mentioned above is that the lowest order dispersion of the imaginary parts of the coupling tensors is proportional to −. Willis also demonstrated this proportionality analytically using a Green’s function approach [33,34]. As time derivatives in the frequency domain may be substituted by multiplication by −, this form suggests a time derivative operation on the field variable may be hidden within the effective Willis coupling coefficient. This conclusion is supported by a simple model of a one-dimensional multi-degree of freedom ‘particle’ with inherently asymmetric microstructure, such as the one shown in appendix A. Analysis of that particle predicts that stress is related to the acceleration rather than the velocity, and the momentum density is related to the strain rate rather than the strain. Furthermore, Nassar et al. also suggested that the low-order dispersion predicted by their model of Willis coupling was actually a time derivative on the field quantities being wrapped into the material property in the frequency domain [14]. Following these suggestions, the reciprocal Willis equations (equations (2.1) with S~ijk=Sjki) can be re-written in the form

σij=CijklεklSijkiωv˙k 4.10a

and

μi=Sjkiiωε˙jk+ρijvj. 4.10b

Then, defining Ψijk=−Sijk/, one obtains a new set of constitutive equations

σij=Cijklεkl+Ψijkv˙k 4.11a

and

μi=Ψjkiε˙jk+ρijvj, 4.11b

where Ψijk is a purely real material property in the low frequency limit that represents Willis coupling. This time domain formulation is particularly interesting because it clearly indicates that the generalized relationships of elastodynamics for stress and momentum degenerate to the common representations if strain and velocity are constant. In other words, the time domain formulation of equations (4.11) implies that Willis coupling is the result of microstructure that does not influence the static stress–strain response of the heterogeneous medium or rigid body dynamics, but that becomes observable under time-varying excitation. This is particularly interesting because it indicates that Willis coupling does not violate Galilean invariance of the stress field in a medium with uniform and constant velocity. As mentioned above, a similar set of constitutive equations were proposed by Nassar et al. after analysing a one-dimensional periodic system of masses and springs [14]. Their proposal was based on the requirement that the imposed stress field be invariant under Galilean transformations and then writing the definition of the momentum in similar manner. Lastly, it is important to note that despite the fact that the time domain formulation was deduced from causality using a highly idealized dispersionless limiting case, Ψijk is not restricted to be dispersionless in general. Indeed, previous work on the topic clearly indicates that this material property may be strongly dispersive when resonant subwavelength material inhomogeneities are present in a medium [9,17].

As equations (4.11) are simply an alternative representation of the Willis equations, the restrictions on Sijk due to passivity may be easily converted to restrictions on Ψijk (the restrictions imposed by reciprocity are implicitly already included). In particular, for a reciprocal and passive system we require

ω|εijΨijkvk|εijCijklεkl+viρijvj, 4.12

where we observe that the lossy component of Ψijk is the imaginary part, analogous to the lossy parts of the stiffness and density tensors. Furthermore, using an analysis similar to that given above, the Kramer–Krönig relations for Ψijk may be written as

Ψijk(ω)Ψijk()=2πP0λΨijk(λ)λ2ω2dλ,Ψijk(ω)=2πP0ωΨijk(λ)λ2ω2dλ, 4.13

which is identical in form to the relations in equations (4.8). Thus, in the limiting case of a lossless, passive, reciprocal material, the restrictions derived above imply

Cijkl(ω)=Cijkl(),ρij(ω)=ρij(),Ψijk(ω)=Ψijk(). 4.14

5. Special cases

In this section, additional requirements of material properties for three special cases of particular interest are considered. First, the case of media supporting wave propagation with very low loss is considered. Then, the case of media without any resonances is discussed. Finally, the requirements on the fully general elastodynamic material properties are reduced to the acoustic limit, where neither shear stress nor strain are supported.

(a). Low loss regions

Propagation with low losses in wave energy is an important subject, and much has been written on the topic [24]. If the net power flux through a region is set equal to zero, then

Cijkl=Ψijk=ρij=0. 5.1

As the imaginary parts of the material properties are identically zero, equation (4.7a) requires the real part to be constant in frequency. This result may seem surprising, because there are many examples of effective media constructed of purely lossless components whose effective properties display non-trivial dispersion. Examples include media with resonant inhomogeneities [5,6] and Bloch media [15]. However, these media are based on hidden degrees of freedom, such as shunt resonators which are inherently dispersive [5], or periodic media which account for long-range interactions [15].

While the presence of a band structure precludes the use of the lossless restrictions, Landau & Lifshitz [24] demonstrated that interesting requirements may be found in the lossless regions. If A′′(λ)=0 for λ in some passband, then the principal integral on the right-hand side of equation (4.7a) may be reduced to a normal integral for ω in the passband. Then, taking a derivative with respect to ω, one may write

Aω=2π02λω(λ2ω2)2A(λ)dλ. 5.2

Notice that over the entire range of integration, the integrand in equation (5.2) takes the sign of A′′(λ). But for the stiffness and density, passivity requires the imaginary part of the material properties to keep the same sign for all frequencies. Therefore, the sign of ∂A′/∂ω is the same as the sign of A′′(ω) in the passbands. It should be noted that because passivity only places a restriction on the magnitude of the coupling tensors, a similar statement for the coupling tensors cannot be made.

(b). Relaxing media

In the regions of loss the Kramers–Krönig relations may still yield information about the slope of A′(ω). Assuming non-negligible A′′(ω), O’Donnell et al. [27] were able to expand the principal value integral in equation (4.7b) about the pole in an infinite power series equivalent to

A(ω)=π2ωAωπ324ω33Aω3+. 5.3

For either small ω or for A′′(ω) approximately proportional to ω (a property of relaxing media), the higher-order terms become negligible, and we find the sign of ∂A′/∂ω has the opposite sign of A′′(ω). This holds for all of the material properties, including the coupling terms.

The cases of Landau & Lifshitz [24] and of O’Donnell et al. [27] lead to opposite conclusions, so the situations in which they are applicable should be clearly delineated. First, the two approaches start from different underlying assumptions, and thus are described using different relationships. As Landau & Lifshitz assume very small A′′(ω), they start with the Kramers–Krönig relation for A′(ω). On the other hand, O’Donnell et al. make no assumption on A′′(ω), and use the Kramers–Krönig relation for A′′(ω). Furthermore, O’Donnell et al. tacitly assume the dominant contribution to the principal value integral comes from the pole, which implies there are no resonances of A′(λ) for λ close to ω. An example where this assumption breaks down is a low-loss material displaying band structure due to sub-wavelength resonances. In a passband far from any band gap, the dominant contribution to the integral in equation (4.7b) is the pole, and the limit of O’Donnell et al. holds. However, close to the edge of the passband, the relatively large values of A′′(ω) in the band gap dominate, and the limit of Landau & Lifshitz becomes appropriate. Figure 1 provides an illustration of these two approximations and their approximate domains of applicability.

Figure 1.

Figure 1.

Demonstration of the O’Donnell [27] and the Landau & Lifshitz [24] approximations. The O’Donnell approximation is applicable for slowly varying real part far from sharp imaginary peaks (red region). The Landau & Lifshitz approximation is applicable for low imaginary part near a resonance or near relatively sharp imaginary peaks (blue region).

(c). Acoustic limit

Because of the recently increased interest in acoustic metamaterials, the causal form of the Willis equations, equations (4.11), is specialized here to the fluid case where shear is not supported. Instead of using the Cauchy stress and strain tensors, the acoustic pressure P and the volumetric strain εV, which are both scalars, will be used.

The volumetric strain is defined as the trace of the strain tensor, and the pressure is defined as negative one-third of the trace of the Cauchy stress

εV=trεij=εii 5.4a

and

P=13trσij=σii3. 5.4b

In the limit of acoustic disturbances, the stress and strain are written as σij=−ij and εij=εVδij/3, respectively. Then equations (4.11) become

3P=13CiikkεV+Ψiikv˙k 5.5a

and

μi=13Ψjjiε˙V+ρijvj, 5.5b

where we have taken the trace of the first equation. We now define κCiijj/9 and ψiΨjji/3 so that we may write

P=κεV+ψiv˙i 5.6a

and

μi=ψiε˙V+ρijvj. 5.6b

For a passive and reciprocal medium, we require κ′′≤0, the requirements on ρij do not change, and the passivity restrictions on the coupling parameter are given by

ω{εVψivi}|εV|2κ+viρijvj. 5.7

Additionally, the limits discussed in §5a still apply.

6. Conclusion

Restrictions on the range of physically meaningful Willis material properties have been derived based on the principles of reciprocity, passivity and causality. These restrictions are summarized in table 1. Reciprocity leads to minor symmetries of the stiffness and coupling tensors. Passivity leads to restrictions on the imaginary parts of the stiffness and mass density tensors and the real parts of the coupling tensors. Causality results in the Kramers–Krönig equations and relate the dispersion relations of the real and imaginary parts of the material properties. The standard representation of the linear Willis constitutive equations is shown to be acausal, and potential alternative representations have been presented.

Table 1.

Summary of the physical restrictions imposed on Willis material properties. The form of the Willis equations corresponding to the causal coupling coefficient Ψijk given here is presented in equations (4.11).

property symbol reciprocity passive and reciprocal
stiffness Cijkl Cijkl=Cklij ℑ{Cijkl}≤0
mass density ρij ρij=ρji ℑ{ρij}≥0
coupling Sijk, S~ijk S~ijk=Sjki ℜ{Sijk} bounded
causal coupling Ψijk=Sijkiω implicitly included ℑ{Ψijk} bounded

Acknowledgements

The work for this paper was performed independently by the authors.

Appendix A. One dimensional asymmetric fluid

Willis coupling (even) can arise from inherent asymmetry of the microstructure of a material [10,15]. To demonstrate this, consider an element represented by two unequal masses and a spring between them (figure 2). Let the first mass be m1=ρ1SΔx/2 at x and the second mass be m2=ρ2SΔx/2 at xx, and let the spring have a spring constant k. In these expressions, S is the cross-sectional area and Δx is the width of the fluid element.

Figure 2.

Figure 2.

Simple asymmetric model of a fluid element, consisting of two masses (m1 at position x and m2 at position xx) and a spring with constant k. The pressure P and displacement ξ are evaluated on the boundaries of the element, x and xx.

There are two equations of motion for each of the masses within the fluid element are given by

ρ1Δx2ξ¨(x)=P(x)k(ξ(x)ξ(x+Δx)) A 1

and

ρ2Δx2ξ¨(x+Δx)=P(x+Δx)+k(ξ(x)ξ(x+Δx)), A 2

where ξ(x) is the displacement at the field point, P(x) is the pressure field, and the over-dots denote a time derivative. These equations may be rearranged to yield the equivalent equations

P(x)P(x+Δx)Δx=ρ12ξ¨(x)+ρ22ξ¨(x+Δx) A 3

and

P(x)+P(x+Δx)2=k(ξ(x)ξ(x+Δx))ρ1Δx4ξ¨(x)+ρ2Δx4ξ¨(x+Δx). A 4

Now, expand each function about the point y=xx/2 and neglect terms O[(Δx)2]

P(y)=ρ1+ρ22ξ¨(y)+ρ2ρ12Δx2ξ¨(y) A 5

and

P(y)=ρ2ρ12Δx2ξ¨(y)kΔxξ(y), A 6

where primes denote spatial differentiation. If we approximate ξ′(y) as the volume strain ε(y) and ξ˙(y) as the particle velocity v(y), and noting that −P′(y) is the time derivative of the momentum density μ˙(y) in accordance with the conservation of linear momentum, we may then write these equations in the suggestive form (where the explicit y is not shown)

μ=ρ1+ρ22v+ρ2ρ12Δx2ε˙ A 7

and

P=ρ2ρ12Δx2v˙kΔxε. A 8

From this form, we readily identify the approximate effective density ρ=(ρ1+ρ2)/2, the effective bulk modulus κ=−kΔx, and the (reciprocal, passive and causal) coupling parameter ψx(ρ2ρ1)/4. Note that k=O(1/Δx), so the coupling terms are higher-order expansions of the effective constitutive equations

P=κε+ψv˙ A 9

and

μ=ψε˙+ρv. A 10

Authors' contributions

C.F.S. derived the reciprocity and passivity results for acoustic media, and M.B.M. derived the same and the restrictions due to causality for elastic media. A.A. and M.R.H. provided valuable insight which significantly guided the derivations given.

Conflict of interests

We declare we have no competing interests.

Funding

This work was supported by ONR through MURI Grant No. N00014-13-1-0631.

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