Abstract
The first and foremost task for carbon storage is to find proper locations to permanently store CO2 which are injected into deep saline aquifers. However, fractures in the reservoir as well as channels along the wells form preferential pathways for CO2 transport to make it easily escapes from the reservoir. Various scientific studies, pilot CCS programs and commercial CCS projects have shown that leakage problems will be detrimental to the environment and safety to human race.
Modeling CO2 flow in fractures along the well remains a challenge. In this work, several CO2 pathways are characterized, including fractures in cement, casing and the rock. Discrete Fracture Modeling (DFM), which represents fractures individually and explicitly, is applied to simulate CO2 movement in a saline aquifer. This requires unstructured gridding of the saline formation using Delaunay triangulation and transmissibility evaluation between each pair of adjacent cells. Simulations have been done using General Purpose Reservoir Simulator with a non-neighbor connection list.
Several examples including flows through wellbore failures, sloped layers as well as Hydraulic fractures are presented. Through the simulation results, it is found that near well fractures act as extremely preferential flow paths for CO2 transport. Fracturing would help CO2 retained in the target aquifer.
The main application of the framework presented in this paper is to help those involved in evaluation and planning of possible CO2 storage location selection to identify and quantify possible leakage risks through drilling and completion induced fractures.