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Comment out the biharmonic stuff - its wrong and I will fix it |
Biharmonic equation |
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:<math> \alpha^2=\left(\kappa+\frac{4}{3}\mu\right)/\rho \qquad \beta^2=\mu/\rho </math>
are the [[eigenvalue]]s of <math>A[\hat{\mathbf{k}}]</math> with [[eigenvector]]s <math>\hat{\mathbf{u}}</math> parallel and orthogonal to the propagation direction <math>\hat{\mathbf{k}}</math>, respectively. In the seismological literature, the corresponding plane waves are called P-waves and S-waves (see [[Seismic wave]]).
== The biharmonic equation ==
For a static situation (<math>\partial_t=0</math>) the wave equation becomes a static equation :
:<math>A_{ij}u_j=(\alpha^2-\beta^2)\partial_i\partial_ju_j+\beta^2\partial_k\partial_ku_i=-f_i/\rho</math>
Taking the divergence of both sides of this static equation and assuming a conservative force, (<math>\partial_i f_i=0</math>) we have
:<math>\partial_i A_{ij}u_j = (\alpha^2-\beta^2)\partial_i\partial_i\partial_ju_j+\beta^2\partial_i\partial_m\partial_mu_i = \alpha^2\partial_i\partial_i\partial_ju_j = 0</math>
from which we conclude that:
:<math>\partial_i\partial_i\partial_ju_j = 0</math>
Taking the Laplacian of both sides of the static equation, a conservative force will give <math>\partial_k\partial_kf_i=0</math> and we have
:<math>\
From the divergence equation, the first term on the right is zero and we conclude that:
:<math>\
or, in coordinate free notation <math>\nabla^4 \mathbf{u}=0</math> which is just the [[biharmonic equation]] in <math>\mathbf{u}</math>.
== References ==
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