Modeling variable-density flow in saturated-unsaturated porous media: An advanced numerical model

dc.contributor.authorYounès, Anis
dc.contributor.authorKoohbor, Behshad
dc.contributor.authorBelfort, Benjamin
dc.contributor.authorAckerer, Philippe
dc.contributor.authorDoummar, Joanna
dc.contributor.authorFahs, Marwan
dc.contributor.departmentDepartment of Geology
dc.contributor.facultyFaculty of Arts and Sciences (FAS)
dc.contributor.institutionAmerican University of Beirut
dc.date.accessioned2025-01-24T11:24:17Z
dc.date.available2025-01-24T11:24:17Z
dc.date.issued2022
dc.description.abstractModeling variable-density flow in unconfined aquifers is a challenging task because of the nonlinear coupling between variably saturated flow and contaminant transport. This results in a highly nonlinear system since the strongly nonlinear Richards flow equation is, in addition, coupled to the advection-dispersion transport equation by viscosity and density variation. The solution of such a nonlinear system is often subject to convergence issues and can be very expansive in terms of computational time, especially for large-scale problems. Conventional numerical algorithms based on the sequential approach and the classical finite difference or finite element methods with the first-order backward Euler time integration scheme are generally inefficient and/or do not provide satisfactory results. In this work, we develop a new efficient and accurate 2D numerical model for the transport of dense contaminants in unsaturated porous media that allows for the simulation of large-scale problems. This research describes a new model that combines advanced spatial discretization methods (mixed hybrid finite element method, discontinuous Galerkin finite element method, and multipoint flux approximation method) with higher-order time integration techniques via the method of lines (MOL). The latter allows one to adapt the time step's size and the order of the time integration to improve the computational efficiency while maintaining accuracy. The robustness and accuracy of the new model are shown by comparison against a widely used commercial code based on the standard finite element method. The applicability of the developed model to a large-scale problem is then investigated by simulating saltwater intrusion under a climate change projection and long-term pumping regimes for the Akkar coastal aquifer in Lebanon using a simplified 2D conceptual model. © 2021 Elsevier Ltd
dc.identifier.doihttps://doi.org/10.1016/j.advwatres.2021.104077
dc.identifier.eid2-s2.0-85119620647
dc.identifier.urihttp://hdl.handle.net/10938/25972
dc.language.isoen
dc.publisherElsevier Ltd
dc.relation.ispartofAdvances in Water Resources
dc.sourceScopus
dc.subjectDiscontinuous finite element method
dc.subjectField simulation
dc.subjectMethod of lines
dc.subjectMixed finite element method
dc.subjectMulti-point flux approximation
dc.subjectUnsaturated flow
dc.subjectVariable-density flow
dc.subjectAquifers
dc.subjectClimate change
dc.subjectClimate models
dc.subjectComputational efficiency
dc.subjectDiscrete event simulation
dc.subjectGalerkin methods
dc.subjectHydrogeology
dc.subjectNonlinear equations
dc.subjectNonlinear systems
dc.subjectNumerical methods
dc.subjectNumerical models
dc.subjectPorous materials
dc.subjectLarge-scale problem
dc.subjectMixed finite element methods
dc.subjectModel variables
dc.subjectMulti-points
dc.subjectUnsaturated flows
dc.subjectVariable-density flows
dc.subjectAdvection-diffusion equation
dc.subjectFinite element method
dc.subjectFlow modeling
dc.subjectNumerical model
dc.subjectPorous medium
dc.subjectRichards equation
dc.subjectSaturated medium
dc.subjectUnsaturated medium
dc.titleModeling variable-density flow in saturated-unsaturated porous media: An advanced numerical model
dc.typeArticle

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