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An understanding of oil–water replacement mechanism based on interfacial tension gradient during the well shut-in
- Source :
- Energy Reports, Vol 8, Iss , Pp 4006-4021 (2022)
- Publication Year :
- 2022
- Publisher :
- Elsevier, 2022.
-
Abstract
- Spontaneous imbibition behavior of fracturing fluid retained in reservoirs is considered to be one of the important mechanisms of spontaneous oil–water displacement in tight reservoirs. However, the mechanism of imbibition displacement in oil-wet rocks remains unclear. Inspired by the principle of the Marangoni effect, a mathematical model of oil displacement driven by an interfacial tension gradient in an oil-wet capillary tube was established, and the effects of osmotic pressure and hydraulic mechanical dispersion were coupled in the model. The results show that the key component of this mechanism is the breakdown of the initial capillary equilibrium state due to the diffusion of solute, which changes the pressure distribution in the capillary and drives the water to drive oil out of the pores. This can explain the spontaneous imbibition of low-salinity fracturing fluid into the oil-wet tight sample and displace oil without any external force, despite its low permeability. In addition, the related factors were analyzed, including initial concentration, contact angle, solute type, osmotic behavior, and size of the capillary. The results show that for an oil wet reservoir with high salinity, the connate water interfacial tension gradient plays an important role in oil displacement, and the coupling effect of osmotic pressure and hydromechanical dispersion considerably improves recovery. This can provide new insight into the mechanism of spontaneous imbibition of fracturing fluid.
Details
- Language :
- English
- ISSN :
- 23524847
- Volume :
- 8
- Issue :
- 4006-4021
- Database :
- Directory of Open Access Journals
- Journal :
- Energy Reports
- Publication Type :
- Academic Journal
- Accession number :
- edsdoj.75812675cb9a46ae85ed92b5e1b43b42
- Document Type :
- article
- Full Text :
- https://doi.org/10.1016/j.egyr.2022.03.011