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Geochemical modelling of hydrogen wettability on Quartz: Implications for underground hydrogen storage in sandstone reservoirs
被引:30
|作者:
Zeng, Lingping
[1
]
Keshavarz, Alireza
[2
]
Jha, Nilesh Kumar
[2
]
Al-Yaseri, Ahmed
[3
]
Sarmadivaleh, Mohammad
[1
]
Xie, Quan
[1
]
Iglauer, Stefan
[2
]
机构:
[1] Curtin Univ, WA Sch Mines Minerals Energy & Chem Engn, 26 Dick Perry Ave, Kensington, WA 6151, Australia
[2] Edith Cowan Univ, Sch Engn, 270 Joondalup Dr, Joondalup, WA 6027, Australia
[3] King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Ctr Integrat Petr Res, Dhahran, Saudi Arabia
关键词:
Hydrogen wettability;
Sandstone reservoirs;
Underground hydrogen storage;
Geochemical modelling;
NATURAL-GAS;
SURFACE;
PRESSURE;
ENERGY;
TRANSPORTATION;
SUBSURFACE;
REACTIVITY;
FORCE;
DLVO;
OIL;
D O I:
10.1016/j.molliq.2022.121076
中图分类号:
O64 [物理化学(理论化学)、化学物理学];
学科分类号:
070304 ;
081704 ;
摘要:
Renewable energy particular hydrogen can be optimum solution to replace fossil fuels to achieve net-zero carbon emission targets and metigate global warming. One challenge of the hydrogen industry is to safely and economically store hydrogen. To meet this requirement, underground geological storage is a poten-tially suitable solution to store hydrogen in large-scale and long-term manner. Wettabillity is an impor-tant formation parameter that can affect flow behaviors of stored gas, cycling efficiency, structural and residual trap capacity. However, current research is still scarce in geochemical reactions associated hydrogen wettability alteraction in subsurface sandstone reservoirs under in-situ conditions. To fill this knowledge gap, in this study, we performed surface complexation modelling to understand the wettabil-ity of hydrogen-brine-organic acid-quartz system. The surface potential of pure quartz at various temper-atures and pressure was calculated to characterize disjoining pressure isotherm. Besides, surface species concentrations of quartz and organic stearic acid were predicted to quantify the electrostatic attraction between quartz and organic acid molecues thus the hydrogen wettability on quartz surface. The modelling results show that for pure quartz, increasing temperature and pressure has a negligible effect on disjoining pressure and hydrogen wettability on the pure quartz surface, which is different from the results reported by Iglauer et al., but is in line with the results reported by Hashemi et al. When organic stearic acid is added into system, increasing organic molecules concentration and pressure strengthens the electrostatic attraction of quartz-organic acid and leads to less hydrophilicity and more hydrogen-wetting. This result is consistent with previous contact angle measurements that increasing organic acid concentration increases the brine contact angle, thus the hydrogen wettability. Our work provides a framework to characterize hydrogen wettability on mineral surface using geochemical tools to better assess the feasibility of UHS in depleted sandstone reservoirs.(c) 2022 Elsevier B.V. All rights reserved.
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