A Preliminary Study of the Gas Hydrate Stability Zone in the South China Sea
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A Preliminary Study of the Gas Hydrate Stability Zone in the South China Sea
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    摘要:

    Based on the analysis of sea-bottom temperature and geothermal gradient, and by means of the phase boundary curve of gas hydrate and the sea-bottom temperature versus water depth curve in the South China Sea, this paper studies the temperature and pressure conditions for gas hydrate to keep stable. In a marine environment, methane hydrate keeps stable at water depths greater than 550 m in the South China Sea. Further, the thickness of the gas hydrate stability zone in the South China Sea was calculated by using the phase boundary curve and temperature-depth equations. The result shows that gas hydrate have a better perspective in the southeast of the Dongsha Islands, the northeast of the Xisha Islands and the north of the Nansha Islands for thicker stability zones.

    Abstract:

    Based on the analysis of sea-bottom temperature and geothermal gradient, and by means of the phase boundary curve of gas hydrate and the sea-bottom temperature versus water depth curve in the South China Sea, this paper studies the temperature and pressure conditions for gas hydrate to keep stable. In a marine environment, methane hydrate keeps stable at water depths greater than 550 m in the South China Sea. Further, the thickness of the gas hydrate stability zone in the South China Sea was calculated by using the phase boundary curve and temperature-depth equations. The result shows that gas hydrate have a better perspective in the southeast of the Dongsha Islands, the northeast of the Xisha Islands and the north of the Nansha Islands for thicker stability zones.

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JIN Chunshuang and WANG JiyangInstitute of Geology and Geophysics, Chinese Academy of Sciences, Beijing Strategic Research Center for Oil and Gas Resources, Ministry of Land and Resources, Beijing .2002. A Preliminary Study of the Gas Hydrate Stability Zone in the South China Sea[J]. ACTA GEOLOGICA SINICA(English edition),76(4):

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