Simplifying generalised Wave Equation

In summary, the question is asking for the solution to the Wave Equation in the context of a lecture course on seismic theory for exploration geophysics. The given equation is simplified by assuming constant density and homogeneity, and then further simplified by considering isotropic materials. The final simplified equation differs from the given solution and may require further consideration of the material's properties.
  • #1
BOYLANATOR
198
18

Homework Statement


Please find question attached. The context is a lecture course on seismic theory for exploration geophysics.

Homework Equations


The substitution for the elasticity tensor made in my solution is given in the lecture notes.

Please find my attempt at the solution attached (hopefully readable). For one, I have no idea how to get a negative term in my solution. I wonder if it could be to do with the direction of motion (the sound waves traveling down into the Earth) or perhaps an identity I'm missing.

Thanks in advance for help.
 

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  • #2
BOYLANATOR said:

Homework Statement


Please find question attached. The context is a lecture course on seismic theory for exploration geophysics.

Homework Equations


The substitution for the elasticity tensor made in my solution is given in the lecture notes.

Please find my attempt at the solution attached (hopefully readable). For one, I have no idea how to get a negative term in my solution. I wonder if it could be to do with the direction of motion (the sound waves traveling down into the Earth) or perhaps an identity I'm missing.

Thanks in advance for help.

I know this sounds like a lot of work, but do you think you could transcribe the equations using LaTex or using the provided symbols? It's really helpful for communication in this forum.
 
  • #3
I'll give it a go...

The given Wave Equation is:

[itex] \frac{\partial }{\partial x_j}(C_{ijkl}\frac{\partial u_l}{\partial x_k}) - \frac{\partial^2 (\rho u_i)}{\partial t^2} = 0 .[/itex]​

But we have the simplifications that density is constant in time and that the material is homogeneous. So we can pull out [itex]C_{ijkl} [/itex] and [itex]\rho[/itex] to give:

[itex] C_{ijkl}(\frac{\partial^2 u_l}{\partial x_j \partial x_k}) - \rho \frac{\partial^2 u_i} {\partial t^2} = 0 .[/itex]​

We are then told that the material is isotropic. The lecture material gives an expression for the elastic tensor which is invariant under rotations, i.e. isotropic:

[itex] C_{ijkl} = \lambda \delta_{ij} \delta_{kl} + \mu (\delta_{ij} \delta_{kl} + \delta_{il} \delta_{jk}) [/itex]
Thus, the new Wave Equation is given by:

[itex] \lambda \delta_{ij} \delta_{kl} (\frac{\partial^2 u_l}{\partial x_j \partial x_k}) + \mu (\delta_{ij} \delta_{kl}(\frac{\partial^2 u_l}{\partial x_j \partial x_k})+ \delta_{il} \delta_{jk}(\frac{\partial^2 u_l}{\partial x_j \partial x_k})) =\rho \frac{\partial^2 u_i} {\partial t^2}[/itex]
This simplifies to:

[itex] \lambda \frac{\partial^2 u_k}{\partial x_i \partial x_k} + \mu \frac{\partial^2 u_i}{\partial^2 x_j }+ \mu \frac{\partial^2 u_j}{\partial x_j \partial x_i} =\rho \frac{\partial^2 u_i} {\partial t^2}.[/itex]
This is not the same as the given solution:

[itex] (\lambda + \mu) \frac{\partial^2 u_k}{\partial x_i \partial x_k} - \mu \frac{\partial^2 u_i}{\partial^2 x_i } =\rho \frac{\partial^2 u_i} {\partial t^2}.[/itex]
 

FAQ: Simplifying generalised Wave Equation

What is the generalised wave equation?

The generalised wave equation is a mathematical formula that describes the behavior of waves in a medium. It is a partial differential equation that relates the second derivative of the wave function to its spatial and temporal derivatives.

Why is it important to simplify the generalised wave equation?

Simplifying the generalised wave equation allows us to better understand the behavior of waves in different media and to make predictions about their properties. It also allows us to apply the equation to real-world situations and solve practical problems.

How is the generalised wave equation simplified?

The generalised wave equation can be simplified by making certain assumptions or approximations about the properties of the medium in which the wave is propagating. This can include assuming a homogeneous and isotropic medium, neglecting certain terms in the equation, or using specific boundary conditions.

What are some common applications of the simplified generalised wave equation?

The simplified generalised wave equation is used in a wide range of fields, including acoustics, optics, electromagnetism, and seismology. It is also used in engineering and technology to design and analyze systems that involve wave propagation, such as antennas, sonar, and medical imaging.

Are there any limitations to the simplified generalised wave equation?

Like any mathematical model, the simplified generalised wave equation has its limitations. It may not accurately describe the behavior of waves in complex or non-uniform media, and it may not account for all factors that can affect wave propagation. Therefore, it should be used with caution and its results should be validated with experimental data.

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