Escalating concerns over climate change have accelerated the need to transition towards
cleaner energy sources, such as hydrogen. For a sustainable hydrogen economy, effective
storage solutions are important. Subsurface porous rocks offer a promising solution,
capable of storing substantial volumes of hydrogen for varying durations to meet
fluctuations in energy demand. However, a comprehensive understanding of hydrogen
flow and entrapment within these rocks, particularly under reservoir conditions, remains
a significant challenge.
In this thesis, X-ray micro-tomography is used to investigate the pore-scale distribution,
trapping, and recovery of hydrogen under subsurface conditions. Through 3D flow-visualisation experiments on sandstone rocks, initial and residual hydrogen saturations
are quantified, providing an assessment of the hydrogen storage capacity and recovery
efficiency of these rocks. Additionally, the potential dissolution of hydrogen in brine is
observed, a phenomenon that could contribute to hydrogen loss during storage and
production.
Furthermore, the influence of small-scale rock heterogeneity is investigated through
experiments on a layered rock. These experiments highlight how subtle rock structure
variations impact hydrogen displacement, leading to reduced storage capacity upon
injection and significant hydrogen trapping during production. Such findings stress the
pivotal roles of pore-scale processes and small-scale rock heterogeneity in the design,
selection, and implementation of subsurface hydrogen storage systems.
Moreover, a comparison of experimental results with a pore-network model reveals that
simplistic models fall short in accurately predicting hydrogen flow and trapping in real
rocks, particularly heterogeneous media. This highlights the importance of experimental
research, such as this study, in advancing our understanding and optimisation of
subsurface hydrogen storage.Heriot-Watt University scholarshi
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