Pore-scale network modelling of flow propagators derived from pulsed magnetic field gradient spin echo NMR measurements in porous media

Citation
Ra. Damion et al., Pore-scale network modelling of flow propagators derived from pulsed magnetic field gradient spin echo NMR measurements in porous media, CHEM ENG SC, 55(24), 2000, pp. 5981-5998
Citations number
45
Categorie Soggetti
Chemical Engineering
Journal title
CHEMICAL ENGINEERING SCIENCE
ISSN journal
00092509 → ACNP
Volume
55
Issue
24
Year of publication
2000
Pages
5981 - 5998
Database
ISI
SICI code
0009-2509(200012)55:24<5981:PNMOFP>2.0.ZU;2-G
Abstract
Pulsed magnetic held gradient spin echo (PGSE) NMR experiments carried out on porous media where fluid flow is occurring, may be analysed to give the propagator, P(xi, t), This quantity is the ensemble density distribution of particle (nuclei) displacements in a chosen direction, xi, in a given time interval, t. These displacements arise as a result of both the convection and diffusion of molecules in the flowing fluid. The propagator can be deri ved for various displacement times, t, and hence these gradually probe a wi der domain of the pore-scale velocity field within the porous medium. Such measurements can be performed separately on the oil and water phases in a t wo-phase flowing system. The interpretation and modelling of these single- and two-phase propagators in terms of the pore-scale flow held within the p orous medium presents a difficult and interesting scientific challenge. In this paper, we model the main qualitative features of the experimentally me asured propagators for both single- and two-phase flow using connected 3D p ore network models of porous media. The calculated flow held within such mo dels shows some non-trivial and qualitatively correct predictions about rea l flow fields in porous media. The propagator is modelled directly by incor porating transport due to both convection and diffusion for large numbers o f marker particles (the nuclei) for both single- and two-phase flow. In the latter case, the transport within each of the two immiscible phases (oil a nd water) has been modelled in their separate pore occupancy networks. The network model captures most of the qualitative features for both single- an d two-phase propagators thus giving us the capability to clearly interpret the respective flowing and non-flowing fractions of the oil (non-wetting) a nd water (wetting) phases in two-phase experiments. Therefore, our findings offer a powerful approach - PGSE NMR experiments and associated pore-scale modelling - for understanding and characterising two-phase flow through po rous media. (C) 2000 Published by Elsevier Science Ltd. All rights reserved .