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Radiation of surface Stoneley waves by distributed force sources acting at the solid earth-atmosphere interface

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Abstract

Using the Fourier transform, we find an integral solution describing the excitation of seismoacoustic waves in the solid Earth and the atmosphere by time-dependent forces arbitrarily distributed over the interface between the media. The solid Earth and the atmosphere are modeled by an isotropic solid half-space and a homogeneous gaseous half-space, respectively. Depending on the types of the excited surface and bulk waves, classification of the corresponding force distributions is performed. In the case of harmonic sources, an expression for the period-averaged radiated power of the Stoneley wave is obtained. For arbitrary time dependence of the forces, we find an expression describing the the Stoneley-wave energy radiated during the entire time of the source operation.

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Authors and Affiliations

  1. Radiophysical Research Institute, Nizhny Novgorod, Russia

    A. V. Razin

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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 50, No. 7, pp. 624–637, July 2007.

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Razin, A.V. Radiation of surface Stoneley waves by distributed force sources acting at the solid earth-atmosphere interface. Radiophys Quantum El 50, 570–582 (2007). https://doi.org/10.1007/s11141-007-0050-8

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  • DOI: https://doi.org/10.1007/s11141-007-0050-8

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