Hydrogen wettability of carbonate formations: Implications for hydrogen geo-storage

Mirhasan Hosseini; Jalal Fahimpour; Muhammad Ali; Alireza Keshavarz; Stefan Iglauer

doi:10.1016/j.jcis.2022.01.068

Hydrogen wettability of carbonate formations: Implications for hydrogen geo-storage

J Colloid Interface Sci. 2022 May 15:614:256-266. doi: 10.1016/j.jcis.2022.01.068. Epub 2022 Jan 12.

Authors

Mirhasan Hosseini¹, Jalal Fahimpour², Muhammad Ali³, Alireza Keshavarz³, Stefan Iglauer⁴

Affiliations

¹ Petroleum Engineering Discipline, School of Engineering, Edith Cowan University, 270 Joondalup Dr, Joondalup 6027, WA, Australia. Electronic address: mirhasan.hosseini@gmail.com.
² Department of Petroleum Engineering, Amirkabir University of Technology, Tehran, Iran.
³ Petroleum Engineering Discipline, School of Engineering, Edith Cowan University, 270 Joondalup Dr, Joondalup 6027, WA, Australia.
⁴ Petroleum Engineering Discipline, School of Engineering, Edith Cowan University, 270 Joondalup Dr, Joondalup 6027, WA, Australia. Electronic address: s.iglauer@ecu.edu.au.

PMID: 35101673
DOI: 10.1016/j.jcis.2022.01.068

Abstract

Hypothesis: The mitigation of anthropogenic greenhouse gas emissions and increasing global energy demand are two driving forces toward the hydrogen economy. The large-scale hydrogen storage at the surface is not feasible as hydrogen is very volatile and highly compressible. An effective way for solving this problem is to store it in underground geological formations (i.e. carbonate reservoirs). The wettability of the rock/H₂/brine system is a critical parameter in the assessment of residual and structural storage capacities and containment safety. However, the presence of organic matters in geo-storage formations poses a direct threat to the successful hydrogen geo-storage operation and containment safety.

Experiments: As there is an intensive lack of literature on hydrogen wettability of calcite-rich formations, advancing (θ_a) and receding (θ_r) contact angles of water/H₂/calcite systems were measured as a function of different parameters, including pressure (0.1-20 MPa), temperature (298-353 K), salinity (0-4.95 mol.kg^-1), stearic acid (as a representative of organic acid) concentration (10^-9 - 10^-2 mol/L), tilting plate angle (0° - 45°) and surface roughness (RMS = 341 nm, 466 nm, and 588 nm).

Findings: The results of the study show that at ambient conditions, the system was strongly water-wet, but became intermediate wet at high pressure. The water contact angle strongly increased with stearic acid concentration making the calcite surface H₂-wet. Moreover, the contact angle increased with salinity and tilting plate angle but decreased with temperature and surface roughness. We conclude that the optimum conditions for de-risking H₂ storage projects in carbonates are low pressures, high temperatures, low salinity, and low organic surface concentration. Therefore, it is essential to measure these effects to avoid overestimation of hydrogen geo-storage capacities and containment security.

Keywords: Calcite-rich formation; Contact angle; Hydrogen; Hydrogen geo-storage; Wettability.