POTENTIAL FACTORS INFLUENCING THE FEASIBILITY OF UNDERGROUND HYDROGEN STORAGE IN THE ILLINOIS BASIN
Hydrogen has been successfully stored in solution-mined salt caverns in the United States since the 1980s, but the feasibility of storing hydrogen in siliciclastic formations (e.g., sandstones) is under assessment. Through modeling and batch reaction experiments, recent studies demonstrate that injecting hydrogen into a siliciclastic reservoir might trigger geochemical reactions and/or microbial activity that could lead to hydrogen consumption. Identifying the reactions that might consume hydrogen is critical to determining optimum storage conditions.
The Illinois Basin has been producing hydrocarbons for more than a century. Records show that formations within the basin have also been storing natural gas since the 1950s. The target formations range from Late Cambrian (e.g., Mt. Simon) to Carboniferous (e.g., Cypress) and have been proven to trap natural gas or carbon dioxide. Storing hydrogen underground can be more challenging than other gases due to the physicochemical properties of hydrogen. Therefore, before pumping hydrogen into a depleted reservoir or saline aquifer, it is important to determine optimum reservoir conditions to avoid commodity loss. Research is underway to determine the geochemical reactions that could trigger hydrogen degradation, and to determine the potential of indigenous microbial communities to convert hydrogen into other gases such as methane.