Combination of seismic reflection and constrained resistivity inversion with an application to 4D imaging of the CO2 storage site, Ketzin, Germany

被引:29
|
作者
Bergmann, P. [1 ]
Ivandic, M. [2 ]
Norden, B. [3 ]
Ruecker, C. [4 ]
Kiessling, D. [5 ]
Lueth, S. [1 ]
Schmidt-Hattenberger, C. [1 ]
Juhlin, C. [2 ]
机构
[1] Helmholtz Ctr Potsdam, GFZ German Res Ctr Geosci, Ctr Geol Storage, Potsdam, Germany
[2] Uppsala Univ, Dept Earth Sci, Uppsala, Sweden
[3] Helmholtz Ctr Potsdam, GFZ German Res Ctr Geosci, Reservoir Technol, Potsdam, Germany
[4] Tech Univ Berlin, Dept Appl Geophys, Berlin, Germany
[5] Univ Leipzig, Inst Geol & Geophys, D-04109 Leipzig, Germany
关键词
DATA INCORPORATING TOPOGRAPHY; CO2SINK PROJECT SITE; SURFACE; TOMOGRAPHY; REGULARIZATION; INJECTION; PART; HOLE;
D O I
10.1190/GEO2013-0131.1
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
A combination of seismic and geoelectric processing was studied by means of a structurally constrained inversion approach. Structural constraints were interpreted from the seismic data and integrated into the geoelectric inversion through a local regularization, which allowed inverted resistivities to behave discontinuously across defined boundaries. This arranged seismic processing and constrained resistivity inversion in a sequential workflow, making the generic assumption that the petrophysical parameters of both methods change across common lithostructural boundaries. We evaluated the approach using a numerical example and a real data example from the Ketzin CO2 pilot storage site, Germany. The latter demonstrated the efficiency of this approach for combining 4D seismic and surface-downhole geoelectric data. In consistence with the synthetic example, the constrained resistivity inversions produced clearer delineated images along the boundary between caprock and reservoir formation. Near the CO2 - flooded reservoir, the seismic and geoelectric time-lapse anomalies correlated well. At some distance to the downhole electrodes, however, the geoelectric images conveyed a notably lower resolution in comparison to the corresponding seismic images. Both methods confirm a northwesterly trend for the CO2 migration at the Ketzin site, although a rather northerly direction was initially expected. The results demonstrate the relevance of the presented approach for the combination of both methods for integrated geophysical CO2 storage monitoring.
引用
收藏
页码:B37 / B50
页数:14
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