石油学报 ›› 2006, Vol. 27 ›› Issue (6): 55-59.DOI: 10.7623/syxb200606015

• 地质勘探 • 上一篇    下一篇

砂岩储层地震属性参数对孔隙流体的敏感性评价

邓继新1, 王尚旭2, 李生杰2, 王绪本1   

  1. 1. 成都理工大学信息工程学院 四川成都 610059;
    2. 中国石油大学CNPC物探重点实验室 北京 102249
  • 收稿日期:2005-12-26 修回日期:2006-04-03 出版日期:2006-11-25 发布日期:2010-05-21
  • 作者简介:邓继新,男,1974年9月生,2003年获北京大学博士学位,2005于中国石油大学CNPC物探重点实验室博士后工作期满出站,现为成都理工大学信息工程学院地球物理系教师,主要从事岩石物理、储层地球物理方面的研究.E-mail:xingjia5049@sina.com
  • 基金资助:
    国家重点基础研究规划(973)项目(2001CB209105);中国石化股份有限公司科技重点项目“岩石物理性质综合分析方法研究”部分成果

Sensitivity evaluation of seismic attribute parameters for sandstone reservoir to pore fluid

Deng Jixin1, Wang Shangxu2, Li Shengjie2, Wang Xuben1   

  1. 1. College of Information Engineering, Chengdu University of Technology, Chengdu 610059, China;
    2. CNPC Key Laboratory for Geophysical Prospecting, China University of Petroleum, Beijing 102249, China
  • Received:2005-12-26 Revised:2006-04-03 Online:2006-11-25 Published:2010-05-21

摘要: 对于不同特性的砂岩储层,从地震数据所提取的多种属性参数对孔隙流体变化的响应是有一定差异的。利用统计学原理给出了流体指示因子的计算方法,用于定量评价地震属性参数对孔隙流体变化的响应差异。利用胜利油田沙河街组三段砂岩储层在模拟储层条件下的实验结果,采用属性交会图技术验证了流体指示因子的正确性。对于疏松砂岩及中-高孔隙度固结砂岩,利用纵、横波阻抗差等常规地震属性可较好地判别孔隙含气及饱和水、饱和油状态;而对于致密含气砂岩,纵、横波速度比及泊松比对流体变化相对较为敏感。对于疏松砂岩,由双敏感属性参数所构成的交会图可区分饱和油与饱和水状态,但利用常规属性交会图难以区分固结砂岩孔隙饱和水与饱和油。在准确给出干燥岩石纵、横波速度比的基础上,组合属性参数Ip2-c.Is2相对于常规属性对孔隙流体变化更为敏感,构成的属性交会图对饱和水与饱和油砂岩样品的实验结果具有明显的区分能力。

关键词: 砂岩储层, 地震属性参数, 孔隙流体流动, 敏感性评价, 属性交会图

Abstract: The response of seismic attribute parameters to variation of pore fluid is different for various sandstone reservoirs. A calculation method for fluid indicator is given by the statistical method and used to reflect the response difference of seismic attribute parameters to fluid variation. Experimental results of sandstone reservoir in the third member of Shahejie Formation in Shengli Oil Field proved the applicability of this approach using seismic attributes crossplot technique. According to the calculation results of fluid indicator, the conventional attributes, such as response difference of P wave and S wave, are sufficient for discrimination of gas state in middle-high porosity unconsolidated sandstones and cemented sandstones sample saturated with water and oil. For the tight sandstone containing gas, only velocity ratio of P wave to S wave and Poisson ratio are sensitive to fluid variation. For the unconsolidated sandstones, the crossplot can be used to distinguish saturated oil from saturated water by selecting two sensitive attribute parameters according to their relative values of fluid indicator. For the cemented sandstone, this approach is not applicable. On the basis of exact velocity ratio of P wave to S wave in dry rock, a combined attribute parameter is more sensitive to pore fluid variation than the conventional attributes. The crossplot generated from the combined attribute parameter has an excellent discriminatory capacity for the experimental results of sandstone samples saturated with water and oil.

Key words: sandstone reservoir, seismic attribute parameter, pore fluid flow, sensitivity evaluation, attribute crossplot

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