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Eduardo Kausel-Fundamental solutions in elastodynamics_ a compendium-Cambridge University Press (2006)

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156 Stiffness matrix method for layered media<br />

ωh / π<br />

15<br />

10<br />

5<br />

0<br />

-5<br />

5<br />

10<br />

0<br />

5<br />

15<br />

10<br />

15<br />

Re kh / π Im kh / π<br />

0<br />

Figure 10.3: Wave spectrum for M<strong>in</strong>dl<strong>in</strong><br />

plate, ν = 0.31.<br />

Top: symmetric modes. Bottom: antisymmetric<br />

modes.<br />

ωh / π<br />

15<br />

10<br />

5<br />

0<br />

-5<br />

5<br />

10<br />

0<br />

5<br />

15<br />

10<br />

15<br />

Re kh / π Im kh / π<br />

0<br />

By the way, observe that = ps − q 2 is the Rayleigh function, which is useful for<br />

show<strong>in</strong>g that at high frequencies, the phase velocity of some of these modes converges to<br />

the Rayleigh wave velocity. After f<strong>in</strong>d<strong>in</strong>g the modes, the displacements for the l<strong>in</strong>e load<br />

could be obta<strong>in</strong>ed by modal superposition, very much along the l<strong>in</strong>es of what was done <strong>in</strong><br />

the example <strong>in</strong> Section 9.1. In pr<strong>in</strong>ciple, such superposition must <strong>in</strong>clude both the propagat<strong>in</strong>g<br />

modes and the evanescent modes (real vs. complex eigenvalues or characteristic<br />

wavenumbers k). The exception is when we are <strong>in</strong>terested only <strong>in</strong> the response at some<br />

distance from the source, <strong>in</strong> which case the propagat<strong>in</strong>g modes may suffice. The great<br />

advantage of modal <strong>solutions</strong> is that the <strong>in</strong>verse transforms back <strong>in</strong>to the space doma<strong>in</strong><br />

can be carried out analytically.

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