The Acoustic Properties of Sandy and Clayey Hydrate-Bearing Sediments

Natural gas hydrates samples are rare and difficult to store and transport at in situ pressure and temperature conditions, resulting in difficulty to characterize natural hydrate-bearing sediments and to identify hydrate accumulation position and saturation at the field scale. A new apparatus was designed to study the acoustic properties of seafloor recovered cores with and without hydrate. To protect the natural frames of recovered cores and control hydrate distribution, the addition of water into cores was performed by injecting water vapor. The results show that hydrate saturation and types of host sediments are the two most important factors that govern the elastic properties of hydrate-bearing sediments. When gas hydrate saturation adds approximately to 5-25%, the corresponding P-wave velocity (V-p) increases from 1.94 to 3.93 km/s and S-wave velocity (V-s) increases from 1.14 to 2.23 km/s for sandy specimens; V-p and V-s for clayey samples are 1.72-2.13 km/s and 1.10-1.32 km/s, respectively. The acoustic properties of sandy sediments can be significantly changed by the formation/dissociation of gas hydrate, while these only minorly change for clayey specimens.