A single Rayleigh mode may exist with multiple values of phase-velocity at one frequency

Author:

Forbriger Thomas1,Gao Lingli2,Malischewsky Peter3,Ohrnberger Matthias4,Pan Yudi5ORCID

Affiliation:

1. Karlsruhe Institute of Technology (KIT), Geophysical Institute, Black Forest Observatory (BFO), Heubach 206, 77709 Wolfach, Germany

2. Institute of Applied and Numerical Mathematics, Karlsruhe Institute of Technology (KIT), D-76049 Karlsruhe, Germany

3. Institute of Geosciences, Friedrich-Schiller University Jena, Burgweg 11, 07749 Jena, Germany

4. Institute of Earth and Environmental Sciences, University of Potsdam, Karl-Liebknecht-Straße 24/25, 14476 Potsdam, Germany

5. Geophysical Institute, Karlsruhe Institute of Technology (KIT), 76187 Karlsruhe, Germany

Abstract

SUMMARY Other than commonly assumed in seismology, the phase velocity of Rayleigh waves is not necessarily a single-valued function of frequency. In fact, a single Rayleigh mode can exist with three different values of phase velocity at one frequency. We demonstrate this for the first higher mode on a realistic shallow seismic structure of a homogeneous layer of unconsolidated sediments on top of a half-space of solid rock (LOH). In the case of LOH a significant contrast to the half-space is required to produce the phenomenon. In a simpler structure of a homogeneous layer with fixed (rigid) bottom (LFB) the phenomenon exists for values of Poisson’s ratio between 0.19 and 0.5 and is most pronounced for P-wave velocity being three times S-wave velocity (Poisson’s ratio of 0.4375). A pavement-like structure (PAV) of two layers on top of a half-space produces the multivaluedness for the fundamental mode. Programs for the computation of synthetic dispersion curves are prone to trouble in such cases. Many of them use mode-follower algorithms which loose track of the dispersion curve and miss the multivalued section. We show results for well established programs. Their inability to properly handle these cases might be one reason why the phenomenon of multivaluedness went unnoticed in seismological Rayleigh wave research for so long. For the very same reason methods of dispersion analysis must fail if they imply wave number kl(ω) for the lth Rayleigh mode to be a single-valued function of frequency ω. This applies in particular to deconvolution methods like phase-matched filters. We demonstrate that a slant-stack analysis fails in the multivalued section, while a Fourier–Bessel transformation captures the complete Rayleigh-wave signal. Waves of finite bandwidth in the multivalued section propagate with positive group-velocity and negative phase-velocity. Their eigenfunctions appear conventional and contain no conspicuous feature.

Funder

Deutsche Forschungsgemeinschaft

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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