Variations of internal pressure within reservoirs structurally compartmentalized by sealing faults induce changes in deformations and stresses. If these changes are significant, they can create favorable conditions for fault reactivation by shear or tensile modes. In that scenario, the conditions that develop within reactivated fault zones can trigger potential geomechanical problems such as oil exudation, seismicity and loss of casing integrity. Therefore, it is necessary to forecast the geomechanical behavior of the field and establish limits for pressure changes within the reservoir. This paper deals with a methodology for the evaluation of fault reactivation and fluid migration, using 2D and 3D Finite Element models. In these models, discrete faults are introduced through zero thickness interface elements. The reactivation mechanisms and fluid migration are controlled by the Mohr-Coulomb plastification criterion. 2D and 3D geomechanical models of a field with a set of faults were built in order to compare their predictions. According to the results, different injection pressure limits can be obtained using 2D and 3D models. Furthermore, the 3D configuration of faults that intersect each other can create preferential flow paths for migration of fluids which are not observed in simplified 2D models.
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51st U.S. Rock Mechanics/Geomechanics Symposium
June 25–28, 2017
San Francisco, California, USA
2D and 3D Numerical Modeling of Fault Reactivation Available to Purchase
R. Quevedo;
R. Quevedo
Tecgraf Institute – Pontifical Catholic University of Rio de Janeiro (PUC-Rio)
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M. Ramirez;
M. Ramirez
Tecgraf Institute – Pontifical Catholic University of Rio de Janeiro (PUC-Rio)
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D. Roehl
D. Roehl
Tecgraf Institute and Department of Civil Engineering - PUC-Rio
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Paper presented at the 51st U.S. Rock Mechanics/Geomechanics Symposium, San Francisco, California, USA, June 2017.
Paper Number:
ARMA-2017-0602
Published:
June 25 2017
Citation
Quevedo, R., Ramirez, M., and D. Roehl. "2D and 3D Numerical Modeling of Fault Reactivation." Paper presented at the 51st U.S. Rock Mechanics/Geomechanics Symposium, San Francisco, California, USA, June 2017.
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