Abstract

Subsurface porous formations provide large capacities for underground hydrogen storage (UHS). Successful utilization of these porous reservoirs for UHS depends on accurate quantification of the hydrogen transport characteristics at continuum (macro) scale, specially in contact with other reservoir fluids. Relative-permeability and capillary-pressure curves are among the macro-scale transport characteristics which play crucial roles in quantification of the storage capacity and efficiency. For a given rock sample, these functions can be determined if pore-scale (micro-scale) surface properties, specially contact angles, are known. For hydrogen/brine/rock system, these properties are yet to a large extent unknown. In this study, we characterize the contact angles of hydrogen in contact with brine and Bentheimer and Berea sandstones at various pressure, temperature, and brine salinity using captive-bubble method. The experiments are conducted close to the in-situ conditions, which resulted in water-wet intrinsic contact angles, about 25 to 45 degrees. Moreover, no meaningful correlation was found with changing tested parameters. We monitor the bubbles over time and report the average contact angles with their minimum and maximum variations. Given rock pore structures, using the contact angles reported in this study, one can define relative-permeability and capillary-pressure functions for reservoir-scale simulations and storage optimization.

Highlights

  • Successful transition towards low-carbon energy systems depends on harvesting more renewable resources and on advancements of large-scale (TWh) storage technologies

  • Wettability of the rock in contact with brine and hydrogen plays a crucial role in the displacement processes in underground hydrogen storage (UHS)

  • This paper reports experimental measurements of the contact angle of the hydrogen/brine/sandstone system, relevant for underground hydrogen storage

Read more

Summary

Introduction

Successful transition towards low-carbon energy systems depends on harvesting more renewable resources and on advancements of large-scale (TWh) storage technologies. Renewable energy can be stored in TWh scales, if it is converted into green molecules such as hydrogen. The green hydrogen can be stored in underground geological formations, e.g., in depleted hydrocarbon reservoirs and saline aquifers (Gabrielli et al, 2020; Stone et al, 2009; Rudolph, 2019). UHS in porous formations still remains a challenge, due to lack of characterization data needed as input parameters to perform reservoir simulation and robust storage optimization. Among these input parameters, hydrogen surface properties in contact with reservoir fluids, especially brine, are crucially important (Heinemann et al, 2021)

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call