SPE Journal
Volume 14, Number 4, December 2009, pp. 568-578

SPE-110581-PA

Infinite-Acting Physically Representative Networks for Capillarity-Controlled Displacements

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DOI  More information 10.2118/110581-PA http://dx.doi.org/10.2118/110581-PA

Citation

  • Behseresht, J., Bryant, S.L., and Sepehrnoori, K. 2009. Infinite-Acting Physically Representative Networks for Capillarity-Controlled Displacements. SPE J.  14 (4): 568-578. SPE-110581-PA. doi: 10.2118/110581-PA.

Discipline Categories

  • 6.3.1 Flow in Porous Media
  • 6.3.2 Multi-phase Flow
  • 6.5.1 Simulator Development

Keywords

  • capillary-controlled displacement, drainage, dense random packing of spheres, Delaunay tessellation, periodic (infinite-acting) networks

Summary

Drainage/imbibition simulations are traditionally performed on finite regular lattices. If physically representative networks are used instead, the spatial correlation of pore space features inherent in granular materials is automatically accounted for. However, even these networks are obtained from finite samples, and conditions must be specified on the boundaries. Making the conditions correspond to physically realistic situations is difficult, especially for simulations of phase trapping. This paper presents a method of constructing infinite-acting model rocks, in which a well-defined criterion for phase trapping is possible that is independent of boundary conditions. The foundation of the model is computer-generated dense random periodic packings of spheres. We illustrate the method with simulations of drainage and irreducible wetting-phase saturations. To eliminate possible confounding effects from grains being arranged differently, we compare simulations in infinite-acting networks with simulations in the finite network taken from the unit cell of the periodic packing. Wetting-phase connectivity is assessed globally and accounts for all phase morphologies, including pendular rings.

The drainage endpoint for a finite network was highly sensitive to the number and location of the exit pores; while using the infinite-acting network, we removed this latter sensitivity. Comparison with experiments showed that a strict criterion of wetting-phase connectivity (pores connected only by throats filled with wetting phase) cannot account for typical values of Sw,irr and that connectivity must persist via pendular rings.

Typical laboratory experiments and simulations in finite networks yield drainage curves that approach irreducible wetting phase saturation Sw,irr gradually, with large changes in capillary pressure inducing only small changes in saturation. Simulations in infinite-acting networks do not exhibit this behavior. We argue that these simulations are more representative of behavior in the field and that typical laboratory measurements underestimate the value of Sw,irr.

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History

  • Original manuscript received: 2 August 2007
  • Meeting paper published: 11 November 2007
  • Revised manuscript received: 25 February 2009
  • Manuscript approved: 20 March 2009
  • Published online: 16 July 2009
  • Version of record: 22 December 2009