Speaker
Description
Reactive transport in porous media is of key importance in contaminant hydrology, carbon storage, enhanced oil recovery and chemical reactors engineering. Despite progress made in recent decades, measurement and prediction of the effective reaction rates is still not well understood. In this study we show how flow and transport heterogeneity affects the effective reaction rate. Our approach is based on a reactive transport particle tracking model at the continuum scale, in contrast to the pore-scale models which were successfully used to study the impact of heterogeneity on non-Fickian transport (Bijeljic et al., 2011, 2013) and reactive transport (Pereira Nunes et al., 2016). We make use of our reactive continuous time random walk (CTRW) model that was previously validated using Nuclear Magnetic Resonance (NMR) experimental measurements during dissolution of a Ketton carbonate rock core sample (Oliveira et al., 2021). The CTRW model is defined using a truncated power-law distribution of transit-time, which contains diffusive time cut-off, mean advective time, and a parameter
References
Bijeljic, B., Mostaghimi, P., and Blunt, M. J. (2011). Signature of non-fickian solute transport in complex heterogeneous porous media. Physical Review Letters, 107(20):204502.
Bijeljic, B., Mostaghimi, P., and Blunt, M. J. (2013). Insights into non-Fickian solute transport in carbonates. Water Resources Research, 49(5):2714–2728.
Oliveira, R., Bijeljic, B., Blunt, M. J., Colbourne, A., Sederman, A. J., Mantle, M. D., and Gladden,L. F. (2021). A continuous time random walk approach to predict dissolution in porous media based on validation of experimental NMR data. Advances in Water Resources, page 103847.
Pereira Nunes, J. P., Bijeljic, B., and Blunt, M. J. (2016). Pore-space structure and average dissolution rates: A simulation study. Water Resources Research, 52(9):7198–7212.1
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