EGU24-4162, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-4162
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Impact of an immobile, mobile and permeable phase on mixing-driven reactions in porous media

Joaquin Jimenez-Martinez1,2, Xueyi Zhang1,3, Ishaan Markale1,2, Dorothee Kurz1,2, Zhi Dou3, Maxence Carrel4, Veronica Morales5, and Markus Holzner6
Joaquin Jimenez-Martinez et al.
  • 1Department Water Resources and Drinking Water, Swiss Federal Institute of Aquatic Science and Technology, 8600 Dübendorf, Switzerland
  • 2Department of Civil, Environmental and Geomatic Engineering, ETH Zürich, 8093 Zürich, Switzerland
  • 3School of Earth Sciences and Engineering, Hohai University, 211100 Nanjing , China
  • 4Geopraevent AG, 8045 Zürich, Switzerland
  • 5Department of Civil and Environmental Engineering, University of California Davis, Davis, 95616-5270 California, United States
  • 6Institute of Hydraulic Engineering, Hydraulics and River Research, University of Natural Resources and Life Sciences, 1200 Vienna, Austria

Understanding chemicals mixing and reactions in porous media is critical for many environmental and industrial applications. In the presence of a non-wetting immiscible phase (e.g., gas) within the pore space, it can remain immobile, giving rise to the so-called unsaturated flow, or it can move, resulting in a multiphase flow. In other cases, the immiscible phase can be permeable, as it occurs with biofilms growing within the pore space. We combine experiments and numerical modeling to assess the impact of saturation (fraction of the pore volume occupied by the wetting phase), multiphase flow (stationary two-phase flow), and the presence of permeable biofilm within the pore space on mixing-driven reactions. The product formation is larger for a given flow rate as saturation decreases, while for a given Peclet, it is the opposite. In multiphase flow conditions, for a given flow rate of the wetting phase, the product formation depends on the flow rate of the non-wetting phase. In the presence of biofilms, the product formation is enhanced compared to their absence and is further enhanced with a heterogeneous permeability within the biofilm.

How to cite: Jimenez-Martinez, J., Zhang, X., Markale, I., Kurz, D., Dou, Z., Carrel, M., Morales, V., and Holzner, M.: Impact of an immobile, mobile and permeable phase on mixing-driven reactions in porous media, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4162, https://doi.org/10.5194/egusphere-egu24-4162, 2024.