2.2 Velocity Model Based on Seismic Wave Propagation in Three-phase Effective Medium
Carcione et al[4]use a Biot-type three-phase theory to study the relationship of the velocity of gas hydrate-bearing sediments and the concentration of gas hydrate.Three-phase theory considers the existence of two solids(grain and gas hydrate)and a liquid(water),and a porous matrix containing gas and water.There are three P waves and two S waves based on a three-phase theory proposed by Leclaire et al[6].So there are 5velocities which are solutions of corresponding characteristic equations.Elastic parameters of sediments based on the threephase theory[4]are shown in table 2.
Table 1 Elastic parameters based on weighted time-average and Wood equation[3]
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Table 2 Elastic parameters based on the three-phase theory[4]
