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基于声波速度分析神狐海域水合物垂向分布特征

VERTICAL DISTRIBUTION OF GAS HYDRATE IN SHENHU AREA OF THE SOUTH CHINA SEA BASED ON ACOUSTIC VELOCITY

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【作者】 郭依群乔少华吕万军

【Author】 GUO Yiqun1,2,QIAO Shaohua3,LV Wanjun3(1 China University of Geosciences,Beijing 10083,China;2 Guangzhou Marine Geological Survey,Guangzhou 510760,China;3 China University of Geosciences,Wuhan 430074,China)

【机构】 中国地质大学广州海洋地质调查局

【摘要】 在分析了等效介质理论提出的2种模式的异同点后,结合神狐海域水合物钻井的测井数据与沉积物样品分析数据,基于物理模型的等效介质理论,计算了在不同水合物饱和度条件下的纵波速度,并估算了神狐海域某钻井沉积物孔隙空间中水合物的饱和度,进而分析水合物在沉积物层中的垂向分布特征。研究表明,神狐海域水合物主要分布在190~220 m之间,其饱和度随深度表现为先增大后减小的特点,水合物饱和度最高可达45%。

【Abstract】 The similarities and differences of the two modes raised by the effective medium theory were analyzed.Using the logging data and core samples from the drilling hole in the Shenhu area and based on the equivalent medium theory of a physical model,we estimated the saturation of gas hydrate in pore space of the sediment from a well in Shenhu area and calculated the P-wave velocity on different saturation of gas hydrate.Vertical distribution patterns of the gas hydrate in sediment layer was established.The result shows that the gas hydrate in Shenhu area mainly occurs in the depth of 190~220 m.The gas hydrate saturation increases in the beginning and decreases later on with depth.The highest saturation of the gas hydrate in this area may be as high as 45%.

【基金】 国土资源部公益性科研专项项目(200811014-02);国家重点基础研究发展计划(973)(2009CB219508);国际科技合作计划(2010DFA21740)
  • 【文献出处】 海洋地质前沿 ,Marine Geology Frontiers , 编辑部邮箱 ,2011年07期
  • 【分类号】P631.8
  • 【被引频次】11
  • 【下载频次】307
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