Skip to main content
NIHPA Author Manuscripts logoLink to NIHPA Author Manuscripts
. Author manuscript; available in PMC: 2022 Oct 22.
Published in final edited form as: Phys Med Biol. 2021 Oct 22;66(21):10.1088/1361-6560/ac287e. doi: 10.1088/1361-6560/ac287e

Uniqueness of shear wave modeling in an incompressible, transversely isotropic (ITI) material

Ned C Rouze 1, Anna E Knight 1, Kathryn R Nightingale 1
PMCID: PMC8605801  NIHMSID: NIHMS1752125  PMID: 34544067

Abstract

Five material parameters are required to describe a transversely isotropic (TI) material including two Poisson’s ratios that characterize the compressibility of the material. Both Poisson’s ratios must be specified to model an incompressible, TI (ITI) material. However, a previous analysis of the procedure used to evaluate the incompressible limit in a two-dimensional (2D) space of Poisson’s ratios has shown that elements of the stiffness tensor are not unique in this limit, and that an additional, fourth parameter is required to model these elements for an ITI material. In this study, we extend this analysis to the case of shear wave propagation in an ITI material. Shear wave signals are modeled using analytic Green’s tensor methods to express the signals in terms of the phase velocity and polarization vectors of the shear horizontal (SH) and shear vertical (SV) propagation modes. In contrast to the previous result, the current analysis demonstrates that the phase velocity and polarization vectors are independent of the procedure used to evaluate the 2D limit of Poisson’s ratios without the need to include an additional parameter. Thus, calculated shear wave signals are unique and can be used for comparison with experimental measurements to determine all three model parameters that characterize an ITI material.

Keywords: elastography, shear wave, incompressible, transversely isotropic material

1. Introduction

In a recent study, Knight et al (2021) reported observations of shear wave propagation following an acoustic radiation force impulse (ARFI) excitation in vivo in a vastus lateralis muscle using an excitation configuration in which the muscle fibers were tilted with respect to the plane perpendicular to the excitation axis (see figures 1 and 2 of Knight et al (2021)). Because of the tilted excitation, this configuration enabled the observation of both the shear horizontal (SH) and shear vertical (SV) propagation modes with ultrasound, and thereby allowed the measurement of additional material properties that could not be assessed with the commonly used excitation geometry in which the muscle fibers are not tilted.

Knight et al (2021) analyzed their measurements by comparing the measured shear wave speeds to results from model calculations using a linear, elastic, incompressible, transversely isotropic (ITI) material model. Compared to a transversely isotropic (TI) model, the ITI model takes advantage of the fact that biological tissues are nearly incompressible so that the compressional wave speed is much greater than shear wave speeds, and compressional wave motion can be ignored in the model of shear wave propagation. The ITI material model is derived from a TI model by specifying the values of two Poisson’s ratios required to make the model incompressible, and requires only three material parameters compared to five for the TI model. By observing both SH and SV shear wave propagation, Knight et al (2021) were able to measure all three material parameters, and thereby, obtain a full characterization of muscle as a linear, elastic, ITI material.

One difficulty with the use of an ITI material model is that two Poisson’s ratios must be specified to achieve the incompressible limit, and the procedure used to evaluate the limit in a two-dimensional (2D) space of Poisson’s ratios must be considered. In fact, a previous investigation by O’Donnell and Skovoroda (2004) has shown that elements of the stiffness tensor are not uniquely defined in the incompressible limit, and that an additional, fourth material parameter is required to characterize the material. Thus, this observation raises the question of whether or not a three parameter model is sufficient to characterize an ITI material, and if this model can be used to calculate unique shear wave signals for comparison with experimental measurements.

In this technical note, we review the analysis of O’Donnell and Skovoroda (2004) and extend it to the modeling of shear wave propagation in an ITI material. In particular, we consider the analytical calculation of shear wave signals using Green’s tensor methods (Rouze et al 2020) and the result of these calculations in the limit of an ITI material model. The primary result demonstrated here is that shear wave signals are uniquely defined in the limit of a three-parameter, ITI material model, and thus, measurement of these three parameters is sufficient to fully characterize an ITI material.

2. Incompressible limit of the stiffness matrix for a TI material

Assuming small displacements and a linear stress-strain relation, an anisotropic material can be modeled using a generalized Hooke’s law to relate the stress tensor σ and strain tensor ϵ through a fourth-order stiffness tensor c with components cijkl,

σij=cijklϵkl, (1)

where summation over repeated indices is implied. The stress-strain relation can also be expressed using Voigt notation as a matrix product with a 6 × 6 stiffness matrix C, or compliance matrix S = C−1,

(σ11σ22σ33σ23σ31σ12)=C(ϵ11ϵ22ϵ332ϵ232ϵ312ϵ12)and(ϵ11ϵ22ϵ332ϵ232ϵ312ϵ12)=S(σ11σ22σ33σ23σ31σ12). (2)

In this note, we consider a TI material characterized by an axis of symmetry, A^, such that the material properties are unchanged by reflections across any plane parallel to A^ or rotations about A^. Skeletal muscle is often modeled as a TI material with the symmetry axis determined by the muscle fibers. Five independent parameters are required to specify the stiffness matrix C, or the compliance matrix S, of a TI material (Lai et al 2010). Using the notation L and T to indicate the longitudinal and transverse directions, these five parameters can be expressed (Lai et al 2010, Rouze et al 2020) in terms of six engineering constants using Young’s moduli EL and ET, shear moduli μL and μT, and Poisson’s ratios νLT and νTT along with the relation

μT=ET2(1+νTT). (3)

In terms of these parameters, independent elements C11, C13, C33, C44, and C66 of the stiffness matrix are given by the relations

C11=ET1+νTT1νLT2ET/EL1νTT2νLT2ET/EL,C44=μL,C66=μTC13=ETνLT1νTT2νLT2ET/EL,andC33=EL(1νTT)1νTT2νLT2ET/EL. (4)

The remaining nonzero elements of C are given by symmetry, Cij = Cji, and the relations

C12=C112C66,C22=C11,C23=C13,andC55=C44. (5)

For an ITI material, the dilatation of the material must be zero when subjected to arbitrary stresses. As shown by O’Donnell and Skovoroda (2004) and Rouze et al (2020), this condition requires the two Poisson’s ratios to have specific values,

νLT,inc=12andνTT,inc=1ET2EL. (6)

Thus, three material parameters are required to describe an ITI material. Here, we use the parameters μL, μT, and the ratio R = ET/EL of Young’s moduli as used previously (Rouze et al 2013, Rouze et al 2020). However, with (3) and (6), any three linearly independent combinations of the parameters μL, μT, EL, and ET can be used.

Modeling of an incompressible material can be achieved by considering the limit as the Poisson’s ratios νLL and νLT approach the limiting values (6). As shown in figure 1, this limit can be evaluated in a 2D space of Poisson’s ratios by considering the approach from a position at a distance δ from the limit point along an approach direction specified by an angle α. Using the notation sα = sin α and cα = cos α, the Poisson’s ratios can be expressed relative to the incompressible limits as

νLT=νLT,incδcα=12δcαandνTT=νTT,incδsα=1ET2ELδsα. (7)

Then, the incompressible limit is equivalent to the limit δ → 0.

Figure 1.

Figure 1.

Two dimensional space of Poisson’s ratios for a TI material showing the approach to the incompressible limit point (νLT,inc, νTT,inc) along a trajectory oriented at an angle α relative to the νLT axis. Values of the Poisson’s ratios νLT and νTT can be expressed in terms of α and the distance δ from the limit point using (7).

Elements of the stiffness matrix can be evaluated in the incompressible limit by inserting (7) into (4). From (4), elements C44 and C66 are independent of the Poisson’s ratios and remain constant in the limit. Substituting for ET from (3) and using the ratio R = ET/EL, elements C11, C13, and C33 are given by

C11=2μTD[(1R4)+δcαRδ2cα2R],C13=2μTD{(1R4)+δ[sα2(2R2)cα]+δ2sαcα},andC33=2μTD[(1R4)+δsα(2R1)δ2sα2R] (8)

where the common factor in the denominators of (4) is given by

D=1νTT2νLT2ET/EL=δ(sα+2cαR2cα2Rδ). (9)

Because D is O(δ), elements C11, C13, and C33 diverge in the limit δ → 0. However, the differences between pairs of these elements remain finite,

C11C13δ02μTsα+2cαR[sα2+cα(2+R2)],C11C33δ02μTsα+2cαR[sα(12R)+cαR],andC13C33δ02μTsα+2cαR[sα(122R)+cα(R22)]. (10)

These differences depend on the angle α of approach to the limit point in figure 1. This observation led O’Donnell and Skovoroda (2004) to conclude that three material parameters were not sufficient for a unique description of the stiffness matrix for a ITI material, and that a fourth parameter such as the limit approach angle α was needed to describe the material in the incompressible limit.

We note that expressions similar to (10) for limiting values of the differences in stiffness matrix elements have previously been given by Rouze et al (2020), but that those expressions differ from (10) as they do not depend on the angle α of approach to the limit point. The reason for this disagreement is that Rouze et al (2020) did not consider the possibility that the limit could depend on the direction of approach to the limit point, but instead, set the Poisson’s ratio νTT to its limiting value (6) so that α = 0, and then evaluated the differences (10) in the limit νLT → 1/2. In addition, this same procedure was used to evaluate the limiting value for the phase velocity vSV in expressions (20) of Rouze et al (2013) and (13) of Rouze et al (2020), and also to evaluate the parameters used in the finite element (FE) simulations of wave motion in a nearly ITI (NITI) material in Rouze et al (2013). Thus, results following from those derivations could possibly be affected by the procedure used to evaluate the 2D limit. This possibility is addressed in the following.

3. Modeling shear wave propagation in an ITI material

3.1. Green’s tensor modeling of shear wave propagation in a TI material

In this note, we model shear wave propagation in a linear, elastic, ITI material by calculating shear wave displacements using Green’s tensor methods. As described by Rouze et al (2020), the shear wave displacement u(robs,t) at position robs and time t can be calculated by dividing the excitation source f(rs,ts)=f(rs)W(ts) into source voxels s and summing the contributions from each voxel. The Green’s tensor Gin(robsrs,tts) gives the relative contribution to the signal from each source voxel. Then, in the temporal frequency domain, components ui(robs,ω) of the shear wave displacement can be written as

ui(robs,ω)=sGin(r,ω)fn(rs)W(ω) (11)

where r=robsrs is the relative position between the source and observation positions and summation over the component index n of the force is implied. The Green’s tensor can be calculated as the inverse, 3D Fourier transform of the sum of three terms corresponding to the primary (P) or compressional wave, and the SH, and SV propagation modes, with each term determined by the phase velocity vN and polarization direction P^N for that mode. For the ITI model considered here, we neglect the P-wave mode so that

Gin(r,ω)=N=SH,SV18π3P^iNP^nNρk2vN2ρω2eikrd3k. (12)

where ρ is the material density.

3.2. Phase velocities vN and polarizations P^N in a TI material

The phase velocities vN and polarizations P^N in (12) can be determined by considering plane wave propagation with displacement

u(r,ω)=(PxPyPz)ei(kn^rωt) (13)

where n^ is the propagation direction, k is the wavenumber, and v = ω/k is the speed. To describe the polarization and propagation directions relative to the material symmetry axis, we orient the coordinate system so the z-axis is aligned with A^ and propagation direction is in the xz plane at an angle θ relative to the z-axis so that n^=(sθ0cθ)T where sθ = sin θ and cθ = cos θ. Inserting (13) into the wave equation leads to an eigenequation for the 3×3 matrix Γ with eigenvectors ρv2 and eigenvectors P^ (Tsvankin (2012), Carcione (2015), Rouze et al (2013)),

(C11sθ2+C44cθ20(C13+C44)sθcθ0C66sθ2+C44cθ20(C13+C44)sθcθ0C44sθ2+C33cθ2)(PxPyPz)=ρv2(PxPyPz). (14)

The solution of (14) for the SH propagation mode consists of particle displacements perpendicular to the xz plane,

ρvSH2=μTsθ2+μLcθ2andP^SH=(010), (15)

where C66 = μT and C44 = μL from (4). Note that Rouze et al (2013) refer to this mode as the pure transverse (PT) mode.

Two additional non-trivial solutions of (14) can be found by requiring det (Γ − ρv2I) = 0 where I is the identity matrix. Evaluation of the determinant gives a quadratic equation for the eigenvalues ρv2,

A(ρv2)2+Bρv2+C=0 (16)

where

A=1,B=(C11sθ2+C33cθ2+μL),andC=(C11sθ2+C33cθ2)μL+(C11C33C132)sθ2cθ2(C11+2C13+C33)μLsθ2cθ2. (17)

Then, the phase velocities for the P and SV modes are given by

ρv2=B2±B214CB2. (18)

The polarization vectors for these modes are given by Carcione (2015) and Rouze et al (2013),

P^=1N((C33cθ2+μLsθ2ρv2)1/20(C11sθ2+μLcθ2ρv2)1/2) (19)

where N=(C11sθ2+C33cθ2+μL2ρv2)1/2 is a normalization factor. These solutions correspond to the SV propagation mode (upper sign in (18)) with polarization approximately transverse to the propagation direction n^, and the P propagation mode (lower sign in (18)) with polarization approximately aligned with n^. Rouze et al (2013) refer to these modes as the quasi-transverse (QT) and quasi-longitudinal (QL) modes, respectively.

3.3. Evaluation of vN and P^N for an incompressible, TI material

We can evaluate the phase velocities vN for the P and SV modes in the limit δ → 0 for an incompressible material by expanding the square root in (18),

ρv2=B2±B2[112(4CB2)18(4CB2)2116(4CB2)3+]. (20)

Using (8) and (9), both B and C are O(1/δ) and diverge in the limit δ → 0. Also, terms of the form Cn/Bm are O(δ(mn)) and vanish in the limit δ → 0 for m > n. Then the eigenvalues ρv2 are given by

ρv2=B2±B2CB+O(δ). (21)

For the lower sign in (21), ρv2B and diverges for δ → 0. This solution corresponds to the P propagation mode which describes the compressional wave whose velocity is expected to diverge in an incompressible material.

The upper sign in (21) corresponds to the SV propagation mode so that, using (17),

ρvSV2=limδ0(CB)=limδ0[(C11sθ2+C33cθ2)μLBC11C33C132Bsθ2cθ2+C11+2C13+C33BμLsθ2cθ2]. (22)

We consider the terms in (22) separately. First, using (17) and (8), B is given by

B=(C11sθ2+C33cθ2+μL)=2μTD[(1R4)+O(δ)]μL. (23)

The first term in the limit on the right hand side (RHS) of (22) is given by

(C11sθ2+C33cθ2)μLB=(BμL)μLB=μL+μL2Bδ0μL. (24)

Using (8), the numerator in the second term on the RHS of (22) is given by

(C11C33C132)=(2μTD)2[δ(1R4)(2sαR+4cα)+O(δ2)] (25)

so that, with (9) and (23), the second term on the RHS of (22) is given by

C11C33C132Bsθ2cθ2δ04μTRsθ2cθ2. (26)

Finally, the last term in (22) can be evaluated using (8) and (23),

(C11+2C13+C33)μLBsθ2cθ2=1B2μTD[4(1R4)+O(δ)]μLsθ2cθ2δ04μLsθ2cθ2. (27)

Then, combining (22), (24), (26), and (27) gives

ρvSV2δ0ρvSV,inc2=μL+4(μTRμL)sθ2cθ2. (28)

Thus, this result is independent of the limit approach angle α and agrees with the previous result from Rouze et al (2013) which was evaluated without consideration of the procedure used to evaluate the 2D limit of Poisson’s ratios.

We note that for the special case R = 4, the terms (1 − R/4) vanish in (23), (25), and (27), and the evaluation of ρvSV2 will require higher order terms in δ that lead to dependencies on the approach angle α. From a practical standpoint, this issue does not affect the result found above for two reasons. First, it is unlikely the ratio R = ET/EL = 4 will occur in muscle because we expect ET < EL and R < 1. For example, the measurements of Knight et al (2021) reported the tensile anisotropy in the vastus lateralis muscle to be χE=(ELET)/ET=4.67 with the corresponding value R = 0.18. Second, even if calculations of shear wave displacements with R = 4 are required, they can be performed using a value of R that is arbitrarily close to 4. In effect, this approach is equivalent to saying that we can evaluate the incompressible limit to obtain (28) with R ≠ 4, and then apply the result with R = 4.

Polarization vectors for the P and SV modes can be determined by defining a polarization angle ϕ relative to the z-axis, so that, using (19),

tanϕ=PxPz=(C33cθ2+μLsθ2ρv2)1/2(C11sθ2+μLcθ2ρv2)1/2 (29)

From (28) and (8), ρvSV2 remains finite in the incompressible limit while C33 and C11 both diverge, and

ϕSVδ0ϕSV,inc=tan1(cθsθ)=tan1(sin(θπ/2)cos(θπ/2))=θπ/2. (30)

For the P mode, the lower sign in (21) gives ρv2B so that, with (17) and (8),

ϕPtan1[(C33cθ2+μLsθ2+B)1/2(C11sθ2+μLcθ2+B)1/2]δ0tan1(sθcθ)=θ. (31)

Thus, in the incompressible limit, the polarization vectors of the SV and P modes are perpendicular and parallel to the propagation direction, respectively. This result agrees with the result of Rouze et al (2013) which was evaluated without consideration of the approach direction α in the evaluation of the 2D limit of Poisson’s ratios.

4. Discussion and conclusion

The key result of the analysis presented in section 3 is that, in the limit of an ITI material, the phase velocity vSV and polarization P^SV for the SV propagation mode are independent of the procedure used to evaluate the incompressible limit. Thus, these quantities are unique, and shear wave signals calculated using Green’s tensor methods are also unique and can be used for comparison with experimental measurements to characterize the material using a linear, elastic, ITI material model. In particular, this result demonstrates that previous observations of non-unique elements of the stiffness tensor by O’Donnell and Skovoroda (2004) do not extend to the modeling of shear wave propagation in an ITI material.

In fact, it might be argued that models of shear wave propagation in an ITI material should not depend on the procedure used to evaluate the incompressible limit because compressional wave propagation, which depends on the compressibility of the material through the Poisson’s ratios νLT and νTT, is excluded in the model. Instead, the ITI model considers only shear wave motion which is an isovolumetric process and is not dependent on the material compressibility or Poisson’s ratios.

On the other hand, nearly ITI (NITI) material models (Pitre et al (2020), Rouze et al 2013) include compressional wave propagation using a five-parameter, TI material model and set the Poisson’s ratios νLT and νTT near to the values required in the incompressible limit. For example, in their FE modeling of shear wave propagation in a NITI material, Rouze et al (2013) set the Poisson’s ratios to the values νTT = νTT,inc and νLT = 0.499 so that δ = 0.001 and α = 0 in (7). At the same time, μL, μT, and the ratio R = ET/EL were set to the specific values to be modeled, and individual values of EL, ET needed for the FE simulations were calculated using (3) and (6). An alternative approach with, for example, a different approach angle α, would be expected to give essentially identical results for the shear wave signals, with similar, but different, results for the compressional wave signals.

In conclusion, this note addresses the question raised by O’Donnell and Skovoroda (2004) regarding the number of parameters required to characterize the stiffness tensor in an incompressible, transversely isotropic (ITI) material, and the extension of this question to the case of shear wave propagation in these materials. Beginning with a five-parameter, TI material model, O’Donnell and Skovoroda (2004) found that, even with two Poisson’s ratios specified by values consistent with the incompressible limit, three material parameters were not sufficient to describe the stiffness tensor of an ITI material, and instead, a fourth parameter was required to describe the approach to the incompressible limit in a 2D space of Poisson’s ratios. In contrast, the analysis presented in this note demonstrates that three material parameters are sufficient to uniquely characterize shear wave propagation in an ITI material. Thus, analysis of experimentally observed shear wave signals by comparison with calculated signals based on an ITI model are sufficient to determine all three parameters necessary to characterize the material using a linear, elastic, ITI model.

Acknowledgments

The authors thank John J. Pitre Jr., Ivan Pelivanov, and Matthew O’Donnell for raising the question considered in this note and for valuable discussions related to the use of an ITI material model. This work was supported in part by NIH grants R01-EB022106 and R01-CA142824.

References

  1. Carcione JM 2015. Wave fields in real media: wave propagation in anisotropic, anelastic, and porous media, 3rd Ed. (Waltham, MA: Elsevier; ) chap 1 [Google Scholar]
  2. Knight AE, Trutna CA, Rouze NC, Hobson-Webb LD, Caenen A, Jin FQ, Palmeri ML and Nightingale KR 2021. Full characterization of in vivo muscle as an elastic, incompressible, transversely isotropic material using ultrasonic rotational 3D shear wave elasticity imaging IEEE Trans. Med. Imag DOI 10.1109/TMI.2021.3106278 [DOI] [PMC free article] [PubMed] [Google Scholar]
  3. Lai M, Rubin D and Krempl E 2010. Introduction to Continuum Mechanics, 4th Ed. (Burlington, MA: Butterfield-Heineman; ) [Google Scholar]
  4. O’Donnell M and Skovoroda AR 2004. Prospects for Elasticity Reconstruction in the Heart IEEE Trans. Ultrason. Feroelectr. Freq. Control 51 322–8 [PubMed] [Google Scholar]
  5. Pitre JJ, Kirby MA, Li DS, Shen TT, Wang RK, O’Donnell M and Pelivanov I 2020. Nearly-incompressible transverse isotropy (NITI) of cornea elasticity: model and experiments with acoustic micro-tapping OCE Scientific Reports 10 12983. [DOI] [PMC free article] [PubMed] [Google Scholar]
  6. Rouze NC, Wang MH, Palmeri ML and Nightingale KR 2013. Finite element modeling of impulsive excitation and shear wave propagation in an incompressible, transversely isotropic medium J. Biomech 46 2761–8 [DOI] [PMC free article] [PubMed] [Google Scholar]
  7. Rouze N, Palmeri M and Nightingale K 2020. Tractable calculation of the Green’s tensor for shear wave propagation in an incompressible, transversely isotropic material Phys. Med. Biol 65 1–17 [DOI] [PMC free article] [PubMed] [Google Scholar]
  8. Tsvankin ID 2012. Seismic signatures and analysis of reflection data in anisotropic media (Geophysical Reference Series no 19) ed Gaiser J and Fomel S (Tulsa, OK: Society of Exploration Geophysicists; ) chap 1 [Google Scholar]

RESOURCES