Simplifying generalised Wave Equation

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SUMMARY

The discussion centers on the simplification of the generalized wave equation in the context of seismic theory for exploration geophysics. The original wave equation involves the elasticity tensor and density, which are simplified under the assumptions of constant density and isotropic material. The participants analyze the transformation of the wave equation, leading to a new expression that incorporates the elastic constants λ and μ. The discrepancy between the derived solution and the expected solution highlights the importance of correctly applying the properties of isotropy and the elasticity tensor.

PREREQUISITES
  • Understanding of wave equations in physics
  • Familiarity with elasticity tensors and their properties
  • Knowledge of isotropic materials in geophysics
  • Proficiency in LaTeX for mathematical notation
NEXT STEPS
  • Study the derivation of the wave equation in isotropic media
  • Learn about the properties of elasticity tensors and their applications
  • Explore the implications of constant density in wave propagation
  • Practice transcribing complex equations using LaTeX
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Students and professionals in geophysics, particularly those focusing on seismic theory and wave propagation, as well as educators teaching related concepts in physics and engineering.

BOYLANATOR
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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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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.
 
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]
 

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