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Articles

Experimental and numerical study on fracture propagation near open-hole horizontal well under hydraulic pressure

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Pages 412-430 | Received 25 Oct 2014, Accepted 02 Apr 2015, Published online: 18 May 2015
 

Abstract

Using a true triaxial compression test apparatus, physical model tests are carried out to investigate the fracture propagation in open-hole horizontal wells under hydraulic pressure. The test results indicate that hydraulic fracture propagation is closely related to the direction of the minimum principal stress. When the difference between the maximum and minimum horizontal stresses is maintained at 10.0 MPa and the angle between the horizontal well and the minimum horizontal stress varies from 0° to 90°, the fracturing pattern changes from transversal to longitudinal fractures. To capture the complex hydraulic fractures in heterogeneous rock materials, a three-dimensional numerical code incorporating the seepage-stress-damage coupled model is then employed to study the hydraulic fracture propagation near open-hole horizontal wells. The fracture propagation in horizontal wells under hydraulic fracturing is simulated and the numerical results are in good agreement with the experimental results. The stress distribution, failure-induced stress redistribution and the energy distribution, which are impossible to be observed in field and are difficult to be considered with static stress analysis approaches, are illustrated and discussed in detail based on numerical results. The experimental and numerical results in this study are expected to provide a meaningful guidance for oil production by hydraulic fracturing in horizontal wells.

Acknowledgements

The study presented in this study was jointly supported by grants from PetroChina Innovation Foundation (Grant No. 2013D-5006-0211) and National Natural Science Foundation of China (Grant No. 51479024). The authors are grateful for these supports.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

This work was supported by the PetroChina Innovation Foundation [grant number 2013D-5006-0211]; National Natural Science Foundation of China [grant number 51479024].

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