Consider the Love-wave model of this chapter: a layer of thickness and shear speed…

PHYSICS · Multi-part · Fermi University Physics · Oscillations, Waves & Acoustics · Earth, Climate & Energy Physics · Seismology, tectonics and geodynamics

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Problem

Consider the Love-wave model of this chapter: a layer of thickness HH and shear speed vS1v_{S1} welded to a half-space of shear speed vS2>vS1v_{S2} > v_{S1}, with the Love-wave dispersion relation tan⁡ ⁣(ωH1vS12−1c2)=μ21/c2−1/vS22μ11/vS12−1/c2 ,vS1<c<vS2.\tan\!\left(\omega H\sqrt{\frac{1}{v_{S1}^2}-\frac{1}{c^2}}\right) = \frac{\mu_2\sqrt{1/c^2-1/v_{S2}^2}}{\mu_1\sqrt{1/v_{S1}^2-1/c^2}}\,,\qquad v_{S1}<c<v_{S2}. The chapter solves this for the lowest root only, the fundamental mode, and states that a family of higher roots exists at shorter periods without finding them. ((a)) Write x=ωH1/vS12−1/c2x=\omega H\sqrt{1/v_{S1}^2-1/c^2}. The fundamental branch has 0<x<π/20<x<\pi/2. Explain why a second branch, π<x<3π/2\pi<x<3\pi/2, also solves the dispersion relation (the right-hand side is always positive for vS1<c<vS2v_{S1}<c<v_{S2}), and why this branch describes the first higher (overtone) Love mode. ((b)) Show that this first higher mode exists only above a cutoff angular frequency ω1\omega_1, found by setting x=πx=\pi at the point where c→vS2c\to v_{S2} (the right-hand side vanishes there), and that the corresponding cutoff period is T1=2H1vS12−1vS22.T_1 = 2H\sqrt{\frac{1}{v_{S1}^2}-\frac{1}{v_{S2}^2}}. ((c)) Evaluate T1T_1 for the continental model of this chapter, H=35 kmH=35\,\mathrm{km}, vS1=3.5 km s−1v_{S1}=3.5\,\mathrm{km\,s^{-1}}, vS2=4.5 km s−1v_{S2}=4.5\,\mathrm{km\,s^{-1}}, and say whether the T=20 sT=20\,\mathrm{s} wave computed in the text for this model could be mistaken for the first higher mode instead of the fundamental.

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