2021
DOI: 10.1016/j.petrol.2021.109081
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Hydrogen wettability of quartz substrates exposed to organic acids; Implications for hydrogen geo-storage in sandstone reservoirs

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Cited by 105 publications
(44 citation statements)
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“… 14 , 15 Therefore, the behavior of injected hydrogen should be investigated in terms of mobility and multiphase properties to ensure recovery efficiencies are maintained. 16 , 18 (ii) Hydrogen acts as an electron donor for a variety of microbial processes. The occurrence and behavior of hydrogenotrophic microbes must be investigated to determine the impact of potential hydrogen consumption losses and compositional changes of the stored hydrogen.…”
mentioning
confidence: 99%
“… 14 , 15 Therefore, the behavior of injected hydrogen should be investigated in terms of mobility and multiphase properties to ensure recovery efficiencies are maintained. 16 , 18 (ii) Hydrogen acts as an electron donor for a variety of microbial processes. The occurrence and behavior of hydrogenotrophic microbes must be investigated to determine the impact of potential hydrogen consumption losses and compositional changes of the stored hydrogen.…”
mentioning
confidence: 99%
“…43 These sand-packs replicate sandstone reservoirs that are abundant in number and which may serve as potential hydrogen geo-storage media soon. 44 The bulk volume of the sand-pack was 695 mL, and the pore volume (PV) of the sand-packs obtained ranged from 172 to 188 mL. Thus, the sand-packs exhibited a porosity between 24.7 and 27% and a permeability of 484−543 md over various flooding investigations, ensuring that near-similar values were reproducible.…”
Section: Resultsmentioning
confidence: 82%
“…This trend is consistent with that observed in previous research, where the aging of rock surfaces in n-decane/stearic acid solution resulted in the attainment of intermediate water-wet and CO 2 -wet conditions. 20,33,34,77 By contrast, when the quartz and Fontainebleau quartz surfaces are aged in acetone/stearic acid solution and methanol/stearic acid solution, the substrate surfaces are only altered into weakly water-wet conditions at the highest experimental temperature and pressure used herein (323 K and 20 MPa). Under those conditions, the presence of stearic acid/ acetone shifts the advancing and receding contact angles of the non-porous quartz from θ a = 67°and θ r = 61°to θ a = 80°and θ r = 76°(Figure 4d).…”
Section: Effects Of Thementioning
confidence: 93%
“…Similar results have been obtained for the wettability of quartz in CO 2 /brine systems 33 and H 2 /brine environments. 20,49 Generally, the density of CO 2 gas molecules increases with increasing pressure and, hence, the intermolecular interactions between the quartz/Fontainebleau quartz surfaces and the CO 2 gas molecules significantly increase at higher pressure, thereby creating hydrophobic surfaces. 28,37,82 Moreover, although the decrease in gas density with increasing temperature has been found to result in lower contact angles and low CO 2 -wettability of mica, calcite, and shale, 28,36,82,83 the behavior of quartz is quite different.…”
Section: Effects Of Thementioning
confidence: 99%