Porous Rock Storage: Structure and Function
Porous rock storage, also called "rock pore storage", "reservoir storage" or "storage in porous rock formations", are deposits in limestone and sandstone layers. Here, natural gas has accumulated over millions of years. Often, the rock formations used today are depleted natural gas or oil fields. After the end of extraction, these natural gas reservoirs can be converted into underground storage facilities. The porous rock, which previously contained natural gas, absorbs the stored gas like a sponge. The cap of the porous storage consists of a closed rock layer that prevents gas from escaping. Porous rock storage facilities have a storage volume of up to several million cubic meters.
While porous rock storage plays an important role in the long-term storage of natural gas, its use for hydrogen has hardly been investigated so far. The reason: Injection and long-term storage here are quite challenging. Hydrogen is very reactive to organic material and some minerals. This leads to it potentially reacting with surrounding substances and changing chemically during storage, or being contaminated by minerals or residual gases.
Advantages and Disadvantages of Storage Forms
The advantage of cavern storage is that gas can be injected or withdrawn quickly and flexibly. Additionally, one can assume that the stored hydrogen comes out exactly as it went in. Therefore, they are ideal for green hydrogen.
With porous rock storage, on the other hand, it is unclear how pure the withdrawn hydrogen still is. Since impurities can damage equipment in some hydrogen applications, the purity of the gas plays a significant role. Research on hydrogen quality after withdrawal from porous rock storage is still ongoing.