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Constant Q and a fractal, stratifed Earth

By M. Van der Baan

Abstract

Frequency dependent measurements of the quality factor Q typically show a\ud constant behaviour for low frequencies and a positive power law dependence for higher\ud frequencies. In particular, the constant Q pattern is usually explained using intrinsic\ud attenuation models due to anelasticity with either a single or multiple superposed\ud relaxation mechanisms - each with a particular resonance peak.\ud However, in this study, I show using wave localisation theory that a constant\ud Q may also be due to apparent attenuation due to scattering losses. Namely, this\ud phenomenon occurs if the Earth displays fractal characteristics. Moreover, if fractal\ud characteristics exist over a limited range of scales only, even an absorption band can\ud be created - in accordance with observations. This indicates that it may be very\ud difficult to distinguish between intrinsic and scattering attenuation on the basis of\ud frequency dependent measurements of the quality factor only

Year: 2002
OAI identifier: oai:eprints.whiterose.ac.uk:323

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