One of the prominent methods for carbon dioxide sequestration
is
disposal into deep saline aquifers. This is mainly because deep saline
aquifers provide significant capacity for storage of unwanted fluids
underground for a long period. However, saline aquifers may have a
leaky cap rock. The sealing capacity of a cap rock must, therefore,
be evaluated to ensure the integrity and safety of its storage media;
hence robust classifications of the cap rock are required even before
starting the storage/disposal operations. Aqueous fluids can be injected
into a target storage aquifer, and pressure changes owing to leakage
can be monitored in an upper aquifer separated by a cap rock for a
short period. The measurement of pressure responses in the monitoring
aquifer can be used to identify and characterize any leakage path
in the cap rock. This paper provides analytical models in the Laplace
domain for both in situ and ex situ CO2 sequestration methods.
Using the numerical Laplace inverse method called the “Stehfest”
method, the analytical solution in the real domain is calculated.
The analytical solutions developed can be used for determining both
dimensionless pressure changes in monitoring and storage aquifers
due to leakages and dimensionless leakage rates.