ISSN 1004-4140
CN 11-3017/P

AVO信息约束匹配追踪技术在富煤储层刻画中的应用

刘庆文, 秦德文, 胡伟

刘庆文, 秦德文, 胡伟. AVO信息约束匹配追踪技术在富煤储层刻画中的应用[J]. CT理论与应用研究, 2023, 32(2): 189-197. DOI: 10.15953/j.ctta.2022.218.
引用本文: 刘庆文, 秦德文, 胡伟. AVO信息约束匹配追踪技术在富煤储层刻画中的应用[J]. CT理论与应用研究, 2023, 32(2): 189-197. DOI: 10.15953/j.ctta.2022.218.
LIU Q W, QIN D W, HU W. Application of AVO Information-constrained Matching Pursuit Technique in Rich Coal Reservoir Characterization[J]. CT Theory and Applications, 2023, 32(2): 189-197. DOI: 10.15953/j.ctta.2022.218. (in Chinese).
Citation: LIU Q W, QIN D W, HU W. Application of AVO Information-constrained Matching Pursuit Technique in Rich Coal Reservoir Characterization[J]. CT Theory and Applications, 2023, 32(2): 189-197. DOI: 10.15953/j.ctta.2022.218. (in Chinese).

AVO信息约束匹配追踪技术在富煤储层刻画中的应用

基金项目: 中国海油“七年行动计划”东海专项课题(西湖凹陷西部地区勘探开发关键技术研究(CNOOCKJ 135 ZDXM39 SH01));中国海油“十四五”重大科技项目“海上深层/超深层油气勘探技术”(KJGG2022-0402)。
详细信息
    作者简介:

    刘庆文: 男,硕士,中海石油(中国)有限公司上海分公司研究院工程师,主要从事海油石油勘探地球物理研究,E-mail:liuqw3@cnooc.com.cn

    通讯作者:

    刘庆文*,

  • 中图分类号: P  631.4;P  315

Application of AVO Information-constrained Matching Pursuit Technique in Rich Coal Reservoir Characterization

  • 摘要: 针对西湖凹陷富煤环境下储层刻画精度低问题,本文结合煤层AVO截距、梯度特征,提出一种基于AVO信息约束的匹配追踪技术,压制煤层强反射引起的岩性假象,凸显储层真实、有效信号。该方法首先利用煤层4类AVO负强截距<i<P</i<、正强梯度<i<G</i<特点,构建煤层地震敏感因子<i<P</i< - <i<G</i<,放大煤层地震响应,并压制非煤层强振幅影响,实现煤层位置精细定位;在此基础上,将该煤层地震信息作为匹配追踪需要分解、重构的原始信号,利用复地震道分析技术提高信号快速匹配分解的效率,完成煤层强反射解耦。模型试算及实际资料应用表明:匹配追踪技术在精细定位煤层地震响应基础上,提高了匹配追踪算法去煤层强振幅效率;煤层解耦后地震数据较好地凸显储层横向展布变化,提高主力气层的纵向刻画精度。
    Abstract: To address the low accuracy of reservoir characterization in XiHu Sag in a coal-rich environment, this study developed a matching pursuit technology based on AVO information constraints combined with the AVO intercept and gradient characteristics of coal. It can suppress the strong reflectance lithologic artifacts caused by coal and highlight actual and effective reservoir signals. Based on the negative intercept <i<P</i< and positive gradient <i<G</i< of the AVO of coal, the seismic–sensitive factor <i<P</i<–<i<G</i< of coal identification was developed to amplify the seismic response of coal and suppress the high-amplitude response of non-coal. Then, to accurately identify the location of coal, the seismic information of coal was used as the original signal that needs to be decomposed and reconstructed by matching pursuit. Additionally, the efficiency of signal-matching decomposition was improved using the technology of complex seismic track analysis. Finally, the strong reflection elimination of coal was completed. Model trials and practical applications indicate that this method could accurately identify the seismic response location of coal and improve the efficiency of the matching pursuit algorithm. Moreover, the coal-eliminated seismic data can better highlight the lateral distribution changes of the reservoir and improve the vertical characterization accuracy of the main gas layer.
  • 图  1   靶区不同岩性AVO类型

    Figure  1.   AVO type of different lithologies in the target area

    图  2   理论模型匹配追踪去煤层强振幅效果对比

    Figure  2.   Strong reflection elimination comparison of theoretical model based on matching pursuit

    图  3   N-1井匹配追踪去强振幅分析

    Figure  3.   High-amplitude elimination analysis of well N-1 based on matching pursuit

    图  4   靶区P6b层砂体横向展布

    Figure  4.   P6b sandstone distribution of the target area

    图  5   过三口钻井叠加地震及Vp/Vs反演剖面

    Figure  5.   Post-stack seismic and Vp/Vs inversion section through three drilled wells

    图  6   过三口钻井P-G煤层地震敏感因子剖面

    Figure  6.   Seismic sensitive factor P - G of coal identification section through three drilled wells

    图  7   匹配追踪去煤层强振幅前后对比分析

    Figure  7.   High-amplitude elimination comparison before and after matching pursuit

    图  8   去煤层强振幅前后Vp/Vs反演对比

    Figure  8.   Vp/Vs inversion comparison before and after high amplitude elimination

    图  9   去煤层强振幅前后P6b砂体平面展布对比

    Figure  9.   P6b sandstone-distribution comparison before and after high-amplitude elimination

    表  1   靶区不同岩性弹性参数

    Table  1   Elastic parameters of different lithologies in the target area

    岩性  Vp/(m/s)Vs/(m/s)密度/(g/cm3纵波阻抗/
    ((m/s)·(g/cm3))
      泥岩415022202.6510998
      Ⅲ 类砂岩350023752.40 8400
      Ⅱ类a型砂岩460027502.4911454
      Ⅱ类b型砂岩430026102.4710621
      Ⅰ类砂岩530032502.5513515
      煤层290015002.00 5800
    下载: 导出CSV

    表  2   靶区不同岩性截距P、梯度GPG

    Table  2   Intercept P, gradient G, and PG of different lithologies in the target area

    岩性截距P梯度GP-G
        Ⅲ 类砂岩-0.135-0.123-0.012
        Ⅱ类a型砂岩 0.020-0.183 0.203
        Ⅱ类b型砂岩-0.017-0.147 0.130
        Ⅰ类砂岩 0.103-0.357 0.460
        煤层-0.301 0.369-0.670
    下载: 导出CSV
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出版历程
  • 收稿日期:  2022-11-07
  • 修回日期:  2022-12-18
  • 录用日期:  2023-01-10
  • 网络出版日期:  2023-02-14
  • 发布日期:  2023-03-30

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