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Sequential approach to joint flow-seismic inversion for improved characterization of fractured media

Author(s)
Kang, Peter Kyungchul; Zheng, Yingcai; Fang, Xinding; Wojcik, Rafal; McLaughlin, Dennis; Brown, Stephen; Burns, Daniel R; Juanes, Ruben; Fehler, Michael; ... Show more Show less
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Abstract
Seismic interpretation of subsurface structures is traditionally performed without any account of flow behavior. Here we present a methodology for characterizing fractured geologic reservoirs by integrating flow and seismic data. The key element of the proposed approach is the identification—within the inversion—of the intimate relation between fracture compliance and fracture transmissivity, which determine the acoustic and flow responses of a fractured reservoir, respectively. Owing to the strong (but highly uncertain) dependence of fracture transmissivity on fracture compliance, the modeled flow response in a fractured reservoir is highly sensitive to the geophysical interpretation. By means of synthetic models, we show that by incorporating flow data (well pressures and tracer breakthrough curves) into the inversion workflow, we can simultaneously reduce the error in the seismic interpretation and improve predictions of the reservoir flow dynamics. While the inversion results are robust with respect to noise in the data for this synthetic example, the applicability of the methodology remains to be tested for more complex synthetic models and field cases.
Date issued
2016-02
URI
http://hdl.handle.net/1721.1/110485
Department
Massachusetts Institute of Technology. Department of Civil and Environmental Engineering; Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Journal
Water Resources Research
Publisher
American Geophysical Union (AGU)
Citation
Kang, Peter K. et al. “Sequential Approach to Joint Flow-Seismic Inversion for Improved Characterization of Fractured Media: SEQUENTIAL APPROACH TO JOINT FLOW-SEISMIC INVERSION.” Water Resources Research 52.2 (2016): 903–919. © 2016 American Geophysical Union
Version: Final published version
ISSN
0043-1397

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