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• W2108011640 abstract "Prediction of shear-wave velocity plays an important role in seismic modeling, amplitude analysis with offset, and other exploration applications. This paper presents a method for predicting S-wave velocity from the P-wave velocity on the basis of the moduli of dry rock. Elastic velocities of water-saturated sediments at low frequencies can be predicted from the moduli of dry rock by using Gassmann’s equation; hence, if the moduli of dry rock can be estimated from P-wave velocities, then S-wave velocities easily can be predicted from the moduli. Dry rock bulk modulus can be related to the shear modulus through a compaction constant. The numerical results indicate that the predicted S-wave velocities for consolidated and unconsolidated sediments agree well with measured velocities if differential pressure is greater than approximately [Formula: see text]. An advantage of this method is that there are no adjustable parameters to be chosen, such as the pore-aspect ratios required in some other methods. The predicted S-wave velocity depends only on the measured P-wave velocity and porosity." @default.
• W2108011640 created "2016-06-24" @default.
• W2108011640 creator A5038481165 @default.
• W2108011640 date "2006-11-01" @default.
• W2108011640 modified "2023-10-11" @default.
• W2108011640 title "A simple method of predicting S-wave velocity" @default.
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• W2108011640 doi "https://doi.org/10.1190/1.2357833" @default.
• W2108011640 hasPublicationYear "2006" @default.
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