| Article ID | Journal | Published Year | Pages | File Type | 
|---|---|---|---|---|
| 6381135 | Advances in Water Resources | 2013 | 11 Pages | 
Abstract
												The cause of such sensitivity to the capillary-pressure model is studied. Particularly, we focus on how the entry pressure is represented in each model. We examine the mass-transfer processes under gravity-capillary equilibrium, molecular diffusion, convective mixing, and in the presence of small-scale heterogeneities. Laboratory measurement of capillary-pressure curves and some important implementation issues of capillary-pressure models in numerical simulators are also discussed. Most CO2 sequestration simulations in the literature employ one of the two capillary-pressure models. It is important to recognize that these two representations lead to very different predictions of long-term CO2 sequestration.
											Related Topics
												
													Physical Sciences and Engineering
													Earth and Planetary Sciences
													Earth-Surface Processes
												
											Authors
												Boxiao Li, Hamdi A. Tchelepi, Sally M. Benson, 
											