Example Krummhörn
Storage operator Uniper Energy Storage is currently building a new hydrogen cavern storage facility in Krummhörn, Lower Saxony. The “Hydrogen Pilot Cavern - HPC Krummhörn” project is located near Wilhelmshaven, where several electrolysis projects are planned and where large quantities of hydrogen in the form of ammonia could be landed in the future.
Furthermore, the existing natural gas caverns near Krummhörn are currently not in operation, which would interfere with existing natural gas storage operations. Uniper is using an existing well for the project, from which the pilot cavern is being developed. Initially, the facility is still relatively small in size. The gas trader's aim is to show how quickly a new cavern storage facility can be put into operation - this is what interests the first hydrogen customers the most.
Since mid-January, Uniper engineers have been working on the excavation of the cavern, which should be completed in the summer. The opening of the storage facility for a realistic trial operation is planned for August. The site will then be further developed commercially in order to provide the market with a storage capacity of 250 GWh as a first step.
Pore reservoirs
Pore reservoirs, also known as “rock pore reservoirs”, “reservoir storage facilities” or “reservoirs in porous rock formations”, are former natural gas reservoirs in limestone and sandstone layers. Natural gas accumulated here over millions of years and was pumped to the surface by humans at some point. After the end of this extraction, these natural gas reservoirs can be converted into underground storage facilities. Porous rock, which previously contained natural gas, absorbs the stored gas like a sponge. The ceiling of the pore storage facility consists of a closed layer of rock that prevents gas from escaping.
While pore storage facilities play an important role in the long-term storage of natural gas, their use for hydrogen has hardly been investigated to date. The reason for this is that injection and long-term storage are much more challenging than with salt caverns. This is because hydrogen is very reactive towards organic material and some minerals. This means that it can react with surrounding materials and change chemically during storage in porous rock.
The biggest difference between cavern and pore storage is therefore that with an artificially created salt cavern, it can be assumed that the stored hydrogen will come out again. With pore storage, on the other hand, it is unclear how pure the released hydrogen is. Research into this is ongoing.