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http://dx.doi.org/10.7776/ASK.2009.28.5.424

Sound Velocity Property of Sediment Containing Gas Hydrate in the Ulleung Basin, East Sea  

Kim, Gil-Young (한국지질자원연구원 석유해저연구본부)
Yoo, Dong-Geun (한국지질자원연구원 석유해저연구본부)
Ryu, Byong-Jae (한국지질자원연구원 석유해저연구본부)
Abstract
This study investigates the difference of sound velocity (compressional wave velocity) between gas hydrate-bearing sediments and nongas hydrate-bearing sediments in the Ulleung Basin, East Sea. We use a dataset measured from one site in the central part of the Ulleung Basin. Sound velocity for gas hydrate-bearing sediment shows the range from 1600 m/s to 2200 m/s. However, the value for nongas hydrate-bearing sediment is mostly around 1500 m/s, being less than 1400 m/s below 140 m subbottom depth. This trend is probably due to the presence of free gas below BSR (Bottom Simulating Reflector). Gas hydrate-bearing sediments show high value (maximum 150 Ohm-m) of resistivity. The physical properties between gas hydrate-bearing sediment and nongas hydrate-bearing sediment are characterized by the different patterns due to the presence of gas hydrate in comparison with those of marine unconsolidated sediments. Therefore, in order to investigate acoustic and physical properties for gas hydrate-bearing sediments, the study for the occurrence type and the amount of gas hydrates should be conducted simultaneously.
Keywords
Geophysical well logging; Gas hydrate; Sound velocity; Ulleung Basin;
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