“…[20][21][22][23][24][25][26][27] In deep aquifers used for geological storage, H 2 is supposed to be mainly produced from the fermentation of organic molecules and consumed by some sulfate-reducers, homoacetogens and methanogens. 4,[28][29][30] It has long been known that these three functional groups may compete for this resource, 25,[31][32][33] along with other compounds found in underground systems. But the consequences for the storage can be significant: consumption of H 2 (and CO 2 ), production of methane and/or sulfide with modification of the gas quality, pyrite precipitates, toxicity, and even tubing corrosion.…”