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We derive the acoustic wave equation from the stress-strain relationship in tensorial form, we'll start by considering the fundamental equations of motion, the stress-strain relationship, and the constitutive relations for a linear elastic medium. Here's a step-by-step derivation:
1. Stress-Strain Relationship and Hooke's Law
For a linear elastic material, the stress tensor $\sigma_{ij}$ is related to the strain tensor $\epsilon_{ij}$ through Hooke's law:
$\sigma_{ij} = 𝐶_{ijkl} \ \epsilon_{kl}$
Where:
$\sigma_{ij}$ is the stress tensor.
$\epsilon_{ij}$ is the strain tensor.
$𝐶_{ijkl}$ is the fourth-order stiffness tensor that relates stress and strain.
For an isotropic material, Hooke's law simplifies to:
$u_{i}$ is the displacement component in the $i$-th direction.
$x_{j}$ is the position coordinate in the $j$-th direction.
3. Equation of Motion
Newton's second law $(F=ma)$ for a continuous medium gives us the equation of motion, which relates the stress tensor to the acceleration of the displacement:
If we take the divergence of the displacement field $\nabla \cdot u$ and substitute it into the above equation, the acoustic wave equation in an isotropic medium is:
In the special case where the medium is homogeneous and isotropic (same properties in all directions), and assuming small perturbations, this reduces to:
$\boxed{\nabla^2 u - \frac{1}{c^2} \frac{\partial^2 u}{\partial t^2} = 0}$
where $c$ is the speed of sound in the medium, given by $c = \sqrt{\frac{(\lambda + 2\mu)}{\rho}}$
This is the acoustic wave equation for the displacement field $u$ in a homogeneous, isotropic, and linear elastic medium.
Elastic wave equation
To derive the elastic wave equation for an elastic medium, we'll follow a similar process to the acoustic wave equation derivation but consider the vector nature of displacements in an elastic solid. The elastic wave equation describes how mechanical waves propagate through a solid medium and accounts for both longitudinal (compressional) and shear (transverse) waves.
Steps 1 to 3 are the same, also we follow the same procedure. Let's start from step no. 4
4. Substitute Stress-Strain Relationship into the Equation of Motion
Substituting the stress-strain relationship $\sigma_{ij} = \lambda \delta_{ij} \ \epsilon_{kk} + 2\mu \ \epsilon_{ij}$ into the equation of motion gives:
This is the elastic wave equation in an isotropic medium.
8. Interpreting the Elastic Wave Equation
The term $(\lambda + \mu) \nabla(\nabla \cdot u)$ corresponds to the propagation of compressional (longitudinal) waves, also known as P-waves.
The term $\mu \nabla^2 u$ corresponds to the propagation of shear (transverse) waves, also known as S-waves.
The elastic wave equation describes how these two types of waves propagate through a solid medium. The P-wave speed $(c_p)$ and S-wave speed $(c_s)$ are given by:
$c_p = \sqrt{\frac{\lambda + 2\mu}{\rho}}$ and $c_s = \sqrt{\frac{\mu}{\rho}}$
These wave speeds determine how fast the respective wave types travel through the medium.
Hence, the Elastic Wave Equation in Time Domain in vector form for a linear, isotropic, and homogeneous medium is:
To convert the elastic wave equation from the time domain to the frequency domain, we need to perform a Fourier transform on the equation. The Fourier transform allows us to analyze the wave equation in terms of frequency components, which can be particularly useful for solving problems where time-harmonic solutions are desired.