Bayesian inversion of time-lapse seismic data for the estimation of static reservoir properties and dynamic property changes

被引:39
|
作者
Grana, Dario [1 ,2 ]
Mukerji, Tapan [3 ,4 ]
机构
[1] Univ Wyoming, Dept Geol & Geophys, Sch Energy Resources, Laramie, WY 82071 USA
[2] Univ Wyoming, Dept Chem & Petr Engn, Sch Energy Resources, Laramie, WY 82071 USA
[3] Stanford Univ, Dept Energy Resources Engn, Stanford, CA 94305 USA
[4] Stanford Univ, Dept Geophys, Stanford, CA 94305 USA
关键词
Time-lapse studies; 4D; Bayesian inversion; reservoir characterization; rock physics; FLUID SATURATION CHANGES; ROCK-PHYSICS; CLAY CONTENT; PRESSURE; VELOCITIES; POROSITY; PORE; DISCRIMINATION; SENSITIVITY; PARAMETERS;
D O I
10.1111/1365-2478.12203
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Seismic conditioning of static reservoir model properties such as porosity and lithology has traditionally been faced as a solution of an inverse problem. Dynamic reservoir model properties have been constrained by time-lapse seismic data. Here, we propose a methodology to jointly estimate rock properties (such as porosity) and dynamic property changes (such as pressure and saturation changes) from time-lapse seismic data. The methodology is based on a full Bayesian approach to seismic inversion and can be divided into two steps. First we estimate the conditional probability of elastic properties and their relative changes; then we estimate the posterior probability of rock properties and dynamic property changes. We apply the proposed methodology to a synthetic reservoir study where we have created a synthetic seismic survey for a real dynamic reservoir model including pre-production and production scenarios. The final result is a set of point-wise probability distributions that allow us to predict the most probable reservoir models at each time step and to evaluate the associated uncertainty. Finally we also show an application to real field data from the Norwegian Sea, where we estimate changes in gas saturation and pressure from time-lapse seismic amplitude differences. The inverted results show the hydrocarbon displacement at the times of two repeated seismic surveys.
引用
收藏
页码:637 / 655
页数:19
相关论文
共 50 条
  • [31] A study on multiple time-lapse seismic AVO inversion
    Li, JY
    Chen, XH
    Hao, ZJ
    Rui, ZH
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2005, 48 (04): : 902 - 908
  • [32] Continuous models and algorithms for time-lapse seismic inversion
    Chen Yong
    Han Bo
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2006, 49 (04): : 1164 - 1168
  • [33] Sensitivity of time-lapse seismic to reservoir stress path
    Sayers, CM
    GEOPHYSICAL PROSPECTING, 2006, 54 (03) : 369 - 380
  • [34] Neural network for time-lapse seismic reservoir monitoring
    JPT, Journal of Petroleum Technology, 2002, 53 (08): : 44 - 47
  • [35] Study of time-varying reservoir permeability based on time-lapse seismic data
    Guo Q.
    Zhuang T.
    He S.
    Li Z.
    Wei P.
    Liu L.
    Shiyou Diqiu Wuli Kantan/Oil Geophysical Prospecting, 2022, 57 (01): : 176 - 183
  • [36] Modeling a gas condensate reservoir with time-lapse seismic
    Denney, D
    JOURNAL OF PETROLEUM TECHNOLOGY, 2003, 55 (02): : 60 - 61
  • [37] Modeling a gas condensate reservoir with time-lapse seismic
    Waggoner, J.R.
    Cominelli, A.
    Seymour, R.H.
    JPT, Journal of Petroleum Technology, 2003, 55 (02): : 60 - 61
  • [38] Analysis of time-lapse seismic and production data for reservoir model classification and assessment
    Souza, Rafael
    Lumley, David
    Shragge, Jeffrey
    Davolio, Alessandra
    Schiozer, Denis Jose
    JOURNAL OF GEOPHYSICS AND ENGINEERING, 2018, 15 (04) : 1561 - 1587
  • [39] Improved reservoir modelling with time-lapse seismic data in a Gulf of Mexico gas condensate reservoir
    Waggoner, JR
    Cominelli, A
    Seymour, RH
    Stradiotti, A
    PETROLEUM GEOSCIENCE, 2003, 9 (01) : 61 - 71
  • [40] Time-lapse inversion of crosswell radar data
    Day-Lewis, FD
    Harris, JM
    Gorelick, SM
    GEOPHYSICS, 2002, 67 (06) : 1740 - 1752