Holtz, Mark1, Christine Doughty2, Joseph Yeh1, Susan
Hovorka1
(1) The University of Texas at Austin, Austin, TX
(2) LBNL,
ABSTRACT: Modeling of CO2 Saline Aquifer Sequestration and the Effects of
Residual
Phase Saturation
Petrophysical properties have a strong influence on how a plume of injected
CO2 will form and move in the subsurface. Permeability controls the direction and rate of
CO2 movement, and porosity and
residual
saturation control the size, shape, and dispersion. This research simulates the movement of sequestered
CO2 taking into account the effects of
residual
non-wetting phase saturation To examine
CO2 plume characteristics, petrophysical analysis was accompanied by 3D geocellular modeling as an input into fluid-flow simulator. Petrophysical algorithms were developed that captured the interrelationships amoung porosity, horizontal and vertical permeability,
residual
CO2 saturation and wireline logs. These petrophysical algorithms were applied to develop a 3D geocellular aquifer model based on sandstone-body geometry. The resultant model was used to simulate
CO2 injection in a saline aquifer. Two base cases using constant low or high
residual
CO2 saturation were compared with an algorithm employing variable
residual
saturation. In the latter model, the
residual
CO2 saturation of each grid block depended on the initial CO2 saturation of the grid block, resulting in hysteretic relative permeability and capillary pressure curves. During injection, the
CO2 plume was roughly radially symmetric, with permeability variability, depth, and buoyancy affects combining to create a tornado-shaped plume. During the post-injection period, the initial tornado-shaped plume is distorted by permeability variation, dip direction and
residual
saturation. Much greater dispersion of the
CO2 plume occurred when
residual
CO2 saturation was low.
Residual
non-wetting phase saturation therefore is a key factor controlling long term sequestration.
AAPG Search and Discovery Article #90026©2004 AAPG Annual Meeting, Dallas, Texas, April 18-21, 2004.