Underground Hydrogen Storage (UHS) in Aquifers

1. Since, hydrogen no more directly exists as a gas, how easy would it remain to separate hydrogen, either from water, or, from fossil fuels, despite its abundance in the universe?

2. Whether subsurface hydrogen(H2) storage has been tested in a commercial-scale environment – either in deep saline aquifers, or, in depleted oil/gas reservoirs (apart from salt caverns, practiced in Texas/UK), where, temporarily stored hydrogen has been produced back on demand?

3. Whether, saline aquifers, and/or, oil/gas reservoirs, towards H2 storage, is expected to ensure sustainability and resilience of the planned clean hydrogen economy in order to meet the global de-carbonization goal?

4. In the absence of H2 storage, in a thick, porous and permeable saturated subsurface formation (like a salt cavern), will we be able to satisfy required storage capacity and sufficient injectivity for acceptable well operating rates – either in saline aquifers, or, depleted oil/gas aquifers?

5. Whether, UHS is expected to provide storage capacity in order to balance seasonal supply and demand fluctuations; and also, to meet peak demand towards stabilizing the power grid?

6. How exactly to handle

(a)        The enhanced physical risk of hydrogen leakage (higher tendency of H2 to spread laterally in a porous reservoir increases the probability of escape of the stored H2 either through the abandoned/leaky wells or through the leaking faults)?

(b)       Reduced recoverability of stored H2 product – either in depleted oil/gas reservoirs, or, in deep saline aquifers – given the fact that the H2 remains associated with reduced viscosity and enhanced diffusivity (with reference to natural-gas)?

7. Unlike the minimum requirement of cushion gas in salt caverns, to what extent, cushion gas (employed to ensure sufficient pressure maintenance and adequate withdrawal rates) gets factored into the subsurface storage costs in saline aquifers and depleted oil/gas reservoirs?

8. Towards storing hydrogen in depleted oil/gas reservoirs, how easy would it remain to handle the dynamics of reservoir wettability (that impacts H2 injection and storage); viscous fingering (providing means for hydrogen loss); and the reactivity of H2 with the organic constituents of depleted oil/gas reservoirs (including kerogen, residual hydrocarbons and microbes – leading to H2 losses resulting from chemical or microbial interaction)?

9. Whether the greater compressibility of a cushion gas would really improve the H2 production rate @ the end of a production cycle

? 10.                  Whether the application of standard diffusion models would remain to suffice towards the estimation of the amount of H2 lost through dissolution into formation brine; and diffusing away from the aquifer of interest into the overlying caprock?

Suresh Kumar Govindarajan

Professor (HAG)  IIT-Madras

https://home.iitm.ac.in/gskumar/

https://iitm.irins.org/profile/61643

25-July-2024

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