Abstract
In the present paper, the equation of motion for an incompressible transversely isotropic fibre-reinforced elastic solid is derived in terms of a scalar function. The general solution of the equation of motion is obtained, which satisfies the required radiation condition. The appropriate impedance boundary conditions are also satisfied by the solution to obtain the required explicit secular equation for the Rayleigh wave speed. The numerical values of non-dimensional speed of a Rayleigh wave are obtained with the application of Iteration method. The dependence of the non-dimensional wave speed on non-dimensional material parameter and impedance parameters is shown graphically.
1 Introduction
Fibre-reinforced composite concrete structures are significant due to their low weight and high strength. A reinforced composite has the characteristic property where its components act together as a single anisotropic unit till they remain in the elastic condition. During an earthquake, the artificial structures on the surface of the earth are excited which gives rise to violent vibrations in some cases. The material structures which resist the oscillatory vibration are of much interest to engineers and architects. The idea of introducing a continuous self-reinforcement at every point of an elastic solid is given by Belfield et al. [1].
The propagation of time-harmonic elastic waves in a fibre-reinforced composite were studied by Bose and Mal [2]. Scott and Hayes [3] discussed the small vibrations of a fibre-reinforced composite. Scott [4, 5] studied the waves in a fibre-reinforced elastic material. Sengupta and Nath [6] considered the surface waves in fibre-reinforced anisotropic elastic media. The reflection of qP and qSV waves at the free surface of a fibre-reinforced anisotropic elastic half-space was studied by Singh and Singh [7]. Singh [8] obtained the reflection coefficients from the free surface of an incompressible transversely isotropic fibre-reinforced elastic half-space for the case when the outer slowness section is a re-entrant.
Surface waves play an important role in the study of earthquakes, geophysics and geodynamics. Rayleigh waves cause destruction to the structure due to their slower attenuation of the energy than that of the body waves. Surface waves in elastic solids were first studied by Lord Rayleigh [9] for an isotropic elastic solid. The extension of surface wave analysis and other wave propagation problems to anisotropic elastic materials has been the subject of many studies; see, for example ([10–24]).
Impedance boundary conditions mean a linear combination of the unknown functions and their derivatives is prescribed on the boundary. It is common to use impedance boundary conditions in various fields of physics like acoustics and electromagnetism. Rayleigh waves with impedance boundary conditions are significant in many fields of science and technology. However, very little literature on Rayleigh waves with impedance boundary conditions is available. For example, Malischewsky [25] studied Rayleigh waves with Tiersten’s impedance boundary conditions and obtained a secular equation. Godoy et al. [26] studied the existence and uniqueness of Rayleigh waves with impedance boundary conditions. Recently, Vinh and Hue [27] investigated the propagation of Rayleigh waves in an orthotropic and monoclinic half-space with impedance boundary conditions. In this paper, the propagation of Rayleigh wave in an incompressible transversely isotropic fibre-reinforced elastic medium is considered and an explicit secular equation is obtained under impedance boundary conditions. The iteration method is applied to compute the non-dimensional wave speed of a Rayleigh wave. The non-dimensional speed is plotted against a non-dimensional material parameter to show the effect of impedance and transverse isotropy.
2 Equations of motion
We consider an incompressible transversely isotropic fibre-reinforced elastic medium. The constitutive equation explaining the stress-strain response to small deformation of such a material is given by
where ε, σ and I denote the infinitesimal strain and stress tensors and the 3×3 identity tensors, respectively, and e is a unit vector defining the axis of transversely isotropy. In equation (1), p is the hydrostatic pressure required to maintain the incompressibility constraint
In equation (1), μL and μT are longitudinal and transverse shear moduli and μE is a weighted shear modulus, given by
where EL and ET are longitudinal and transverse Young’s moduli.
Consider a Cartesian coordinate system Ox1x2x3, such that Ox1 is parallel to the direction of transversely isotropy, the constitutive relation (1) is written in component form as
Let us consider a transversely isotropic fibre-reinforced elastic material occupying the half-space x2<0, with boundary x2=0. We consider a plane motion in the (x1, x2) plane with displacement components (u1, u2, u3) such that
where t is time.
For an incompressible material, we have
from which we deduce the existence of a scalar function, denoted ψ(x1, x2, t), such that
Using equation (7) and the strain-displacement relation 2εij =ui,j +uj,i , the stress components are written in terms of scalar function ψ and pressure function p as
where p=p(x1, x2, t) is the hydrostatic pressure associated with the incompressibility constraint, and c12=4μE -μT , c22=μT , c32=μL . The requirements of a physically reasonable response ensure that c12, c22 and c32 are all positive.
In absence of body forces, the equations of motion are
which upon using (8)–(10) give
Elimination of p by cross differentiation leads to the following equation of motion
3 Rayleigh waves
We consider the Rayleigh surface waves propagating along the direction x1 and we write ψ in the form
where y=k x2.
Using equation (15) into equation (14), we obtain
Following Godoy et al. [26] and Vinh and Hue [27], the impedance boundary conditions at the surface x2=0 are
where ω=kc is circular frequency of wave. Z1, Z2 are impedance real valued parameters. With the help of equations (9) and (10), the above boundary conditions are written in terms of scalar function and pressure function as
Differentiating (19) with respect to x1 and eleminating the terms in p with the help of (12), we have
In addition to conditions (18) and (20), we need also the following condition on ψ
In terms of ϕ, the conditions (18), (20) and (21) become
The general solution ϕ(y) of equation (16) that satisfies radiation condition (24) is
where A, B are constants and s1, s2 are solutions of following quadratic equation in s2
If the roots s12 and s22 of the quadratic equation (26) are real, then they must be positive to ensure that s1 and s2 can have a positive real part. If they are complex then they are conjugate. In either case, the product s12s22 must be positive and hence a real (surface) wave speed satisfies the inequalities
Using solutions (25) into boundary conditions (22) and (23), we have
For non-trivial solution, we require the determinant of coefficients of the system of equations (28) and (29) to vanish, which after removal of factor (s2-s1), yields the secular equation in implicit form as
In order to make secular equation explicit, we introduce the notation
Then, the secular equation (30) is expressed in explicit form
where
For ξ=4(μE =μL ), the above equation corresponds to isotropic case. In absence of impedance parameters, i.e. for Z1=0 and Z2=0, the secular equation (31) reduces to
The equation (31) has atleast one solution in the interval (0, 1), if
4 Numerical results
Using iteration method, the equation (31) is solved for the non-dimensional wave speed

Variation of non-dimensional speed of a Rayleigh wave against the non-dimensional material constant ξ, when

Variation of non-dimensional speed of a Rayleigh wave against an impedance parameter

Variation of non-dimensional speed of a Rayleigh wave against an impedance parameter
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