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ON THE DETERMINATION OF THE DOWNGOING P‐WAVES RADIATED BY THE VERTICAL SEISMIC VIBRATOR *
Author(s) -
SAFAR M. H.
Publication year - 1984
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1984.tb01107.x
Subject(s) - seismic vibrator , vibrator (electronic) , geology , amplitude , acoustics , seismology , longitudinal wave , seismic wave , stress (linguistics) , phase (matter) , octave (electronics) , wavelength , acceleration , optics , physics , wave propagation , linguistics , philosophy , quantum mechanics , classical mechanics
A bstract It is well recognized that in order to realize the full potential of the Vibroseis technique, one needs to ensure accurate phase locking and a meaningful cross‐correlation. To achieve these two important objectives we require an accurate estimate of the compressional stress wave radiated by the vibrator into the ground. In this paper a simple method (subject of a patent application) is developed for predicting the compressional stress waves radiated by a vertical vibrator. The main feature of the proposed method is that it involves the field measurement of the acceleration of the reaction mass and the baseplate, respectively. The method is illustrated by computing the compressional stress waves generated by a typical vertical vibrator radiating into ice, chalk, sand, and mud. It is shown that for a seismic vibrator radiating into hard ground the pressure of the downgoing P‐wave is 180° out of phase with the baseplate velocity. It is also shown that when the driving force of the seismic vibrator has a flat amplitude spectrum, the amplitude spectrum of the downgoing P‐wave falls off by 6 dB/octave towards low frequencies.