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Change in apparent viscosity of CO sub 2 foam with rock permeability

Journal Article · · SPE (Society of Petroleum Engineers) Reservoir Engineering; (United States)
DOI:https://doi.org/10.2118/20194-PA· OSTI ID:5437786
 [1]; ;  [2]
  1. Rutgers--the State Univ., New Brunswick, NJ (United States)
  2. New Mexico Inst. of Mining and Technology, Socorro, NM (United States). New Mexico Petroleum Recovery Research Center
This paper summarizes new and previous high-pressure experiments measuring the mobility of CO{sub 2} foam in porous rock, including both sandstones and carbonates, with permeabilities ranging from {lt} 1 md to hundreds of millidarcies. Foam mobility is defined here as the ratio of the combined flow rate per unit superficial area to the pressure drop required for simultaneous flow of dense CO{sub 2} and brine/surfactant through the sample and can be expressed in units of millidarcies per centipoise. The measured results, which can also be expressed in terms of the apparent viscosity of the CO{sub 2} foam, give a quantitative basis for the belief that this displacing fluid should be particularly effective in heterogeneous formations. From a macroscopic viewpoint, the CO{sub 2} foam acts like a single fluid with a viscosity equal to the ratio of the rock's brine permeability to the measured mobility. According to the authors results, the apparent viscosity depends on rock permeability in a nonlinear fashion, increasing from a minimum of about 2 cp for the tightest rocks to an apparent maximum of about 1,000 cp for Berea.
OSTI ID:
5437786
Journal Information:
SPE (Society of Petroleum Engineers) Reservoir Engineering; (United States), Journal Name: SPE (Society of Petroleum Engineers) Reservoir Engineering; (United States) Vol. 6:4; ISSN SREEE; ISSN 0885-9248
Country of Publication:
United States
Language:
English