Multicomponent Fluid Flow in Deforming and Reacting Porous Rock in the Earth’s crust: hydro-mechanical-chemical model
- 1Lomonosov Moscow State University, MHC lab, Mech-Math, Moscow, Russia (andreyfrendak@yandex.ru)
- 2Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
- 3Institute of Geology of Ore Deposits, Petrography, Mineralogy and Biochemistry RAS, Moscow, Russia
We propose a coupled hydro-mechanical-chemical model and its 1D numerical implementation. We demonstrate its application to the model filtration of a multicomponent fluid in deforming and reacting host rocks, considering changes in the densities, phase proportions, and the chemical compositions of the coexisting phases.
The numerical results show the propagation of a porosity wave by means of a viscous (de)compaction mechanism accompanied by the formation of an elongated zone with higher filtration properties. After the formation of such a channel, the formation and propagation of the reaction fronts occurs and are associated with the transformation of the mineral composition of the original rock.
How to cite: Frendak, A., Khakimova, L., Aranovich, L., and Podladchikov, Y.: Multicomponent Fluid Flow in Deforming and Reacting Porous Rock in the Earth’s crust: hydro-mechanical-chemical model, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-8862, https://doi.org/10.5194/egusphere-egu24-8862, 2024.
