Cordilleran Section - 106th Annual Meeting, and Pacific Section, American Association of Petroleum Geologists (27-29 May 2010)

Paper No. 4
Presentation Time: 9:30 AM

EFFECT OF GRAVITY, FLOW RATE, AND SMALL SCALE HETEROGENEITY ON MULTIPHASE FLOW OF CO2 AND BRINE


KUO, Chia wei, PERRIN, Jean Christophe and BENSON, Sally M., Stanford University, Stanford, CA 94305, ershaghi@usc.edu

A series of steady state multiphase flow experiments at a range of fractional flows and flow rates have been conducted using Berea Sandstone. Using the multiphase flow simulator TOUGH2 MP, carbon dioxide saturation distributions, average saturations, and pressure gradients across the core were calculated to determine the influences of sub‑core scale heterogeneity, gravity and flow rate on brine displacement efficiency. It is found that measured CO2 saturation patterns can be replicated using simulation models that include spatially varying porosity, permeability and capillary pressure curves, The interplay of viscous, capillary and gravity forces in core flood experiments are also investigated at different Gravity and Capillary numbers representative of those expected for a typical sequestration project (Gravity numbers 1E2~1E6 while Capillary numbers 1E‑6~1E‑10). These dimensionless numbers span the range of conditions expected in the near‑well region to leading of the plume which may be up to 5 km or more from the injection well. Simulations show that the efficiency of brine displacement and saturation distributions during vertical displacement fall into three separate regimes. At high flow rates representative of the near‑well region, the brine displacement efficiency is nearly independent of flowrate. When the Capillary number drops below 1E‑7 and the gravity number is 1800, both the heterogeneous and homogenous cores display flow rate dependent saturation distributions, with brine displacement efficiency dropping by about 80%. Most of this effect is caused by the influence of gravity, as the decrease in brine displacement efficiency is only slightly smaller for heterogeneous cores. At very low capillary numbers, the brine displacement efficiency appears to asymptotically approach a constant value (flowrate independent). The implications of the interplay between viscous, capillary and gravity forces observed in these high resolution simulations on large scale reservoir displacement efficiency are discussed.