Anna Herring’s Post

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Assist. Prof., Civil and Environmental Engineering, UTK

Excited to share our new paper! We conducted a new thermodymics-based analysis of diffusive transport in geologic systems with multiple partially-soluble fluids, focusing on the important cases of CO2 and H2. We show that in the presence of a geothermal gradient, entropic contributions can reverse the direction of diffusion! This was completely counter-intuitive to me and a fascinating result. We predict that for essentially all realistic geologic carbon storage scenarios, diffusion will drive CO2 downwards. For underground hydrogen storage, the picture is more complicated; H2 will likely diffuse upwards but might reverse direction in deep or high-temperature gradient systems. Published in PRE, with Ruotong Huang and Adrian Sheppard: https://lnkd.in/gpDApcYy (an almost identical version is at arXiv: https://lnkd.in/gUGWpQCs)

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" H2 will likely diffuse upwards but might reverse direction in deep or high-temperature gradient systems." WOW !

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