Types of gas hydrates in marine environments and their thermodynamic characteristics

被引:32
|
作者
Chen, Duo-Fu [1 ]
Su, Zheng
Cathles, Lawrence M.
机构
[1] Chinese Acad Sci, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China
[2] Chinese Acad Sci, Gas Hydrate Res Ctr, Guangzhou, Guangdong, Peoples R China
[3] Cornell Univ, Dept Earth & Atmospher Sci, Ithaca, NY 14853 USA
来源
TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES | 2006年 / 17卷 / 04期
关键词
classification; gas hydrate; thermodynamics; methane solubility; hydrate ridge; South China Sea;
D O I
10.3319/TAO.2006.17.4.723(GH)
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The hydrates in marine environment can be grouped into two categories, diffusion gas hydrates and vent gas hydrates. The diffusion gas hydrates occur widely in an area where bottom simulation reflector (BSR) was recorded in seismic profiles, and is a thermodynamic equilibrium system of hydrates and water with dissolved methane within gas hydrate stability zone (GHSZ). The hydrates are buried in a distance apart from the seafloor and are characterized by low concentrations. The vent gas hydrates occur in an area where gas vents out of the seafloor. It is a thermodynamic disequilibrium system of hydrate, water and free gas, occurs in a zone that extends from the base of GHSZ to the seafloor, and is characterized by high concentration. Reported evidences show that these two types of hydrates are possibly occurring in the South China Sea.
引用
收藏
页码:723 / 737
页数:15
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