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COLLEGE OF OCEANOGRAPHY OREGON STATE UNIVERSITY, CORVALLIS, OREGON 97331
Abstract
We study the falloff rate of the coda of acoustic signals after transmission (net forward-scattering) through a stack of thin layers (compared to the wavelength of the signal) with randomly fluctuating impedances. We find that the change in coda energy with time after the first arrival can be modeled as a decaying exponential with falloff rate
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is the center frequency of a frequency band of the coda, x is the source-receiver distance, and
is the standard deviation of the impedance fluctuation in a band centered about 2
. The dependence of the falloff rate of net forward-scattered coda on
and
is opposite to that of single back-scattered coda, and distinguishes the two types of scattering. This article has been cited by other articles:
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D. A. NOVELO-CASANOVA and R. BUTLER High-frequency seismic coda and scattering in the northwest Pacific Bulletin of the Seismological Society of America, June 1, 1986; 76(3): 617 - 626. [Abstract] [PDF] |
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D. R. BAUMGARDT Comparative analysis of teleseismic P coda and Lg waves from underground nuclear explosions in Eurasia Bulletin of the Seismological Society of America, October 1, 1985; 75(5): 1413 - 1433. [Abstract] [PDF] |
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