Elissa Eggenweiler

ORCID: 0000-0001-7966-9505
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Research Areas
  • Lattice Boltzmann Simulation Studies
  • Advanced Mathematical Modeling in Engineering
  • Advanced Numerical Methods in Computational Mathematics
  • Heat and Mass Transfer in Porous Media
  • Groundwater flow and contamination studies
  • Gaussian Processes and Bayesian Inference
  • Probabilistic and Robust Engineering Design
  • Model Reduction and Neural Networks
  • Aerodynamics and Fluid Dynamics Research
  • Enhanced Oil Recovery Techniques
  • Composite Material Mechanics
  • Soil Geostatistics and Mapping
  • Aerosol Filtration and Electrostatic Precipitation
  • Wind and Air Flow Studies
  • Differential Equations and Numerical Methods

University of Stuttgart
2020-2023

Friedrich-Alexander-Universität Erlangen-Nürnberg
2019

Abstract The intrinsic permeability is a crucial parameter to characterise and quantify fluid flow through porous media. However, this typically uncertain, even if the geometry of pore structure available. In paper, we perform comparative study experimental, semi-analytical numerical methods calculate regular structure. particular, use Kozeny–Carman relation, different homogenisation approaches (3D, 2D, very thin media pseudo 2D/3D), pore-scale simulations (lattice Boltzmann method, Smoothed...

10.1007/s11242-021-01586-2 article EN cc-by Transport in Porous Media 2021-04-17

Abstract The correct choice of interface conditions and effective parameters for coupled macroscale free-flow porous-medium models is crucial a complete mathematical description the problem under consideration accurate numerical simulation applications. We consider single-fluid-phase systems described by Stokes–Darcy model. Different sets coupling this model are available. However, these often arbitrary. use large-scale lattice Boltzmann simulations to validate comparison against pore-scale...

10.1007/s10596-020-09994-x article EN cc-by Computational Geosciences 2020-09-05

Related DatabasesWeb of Science You must be logged in with an active subscription to view this.Article DataHistorySubmitted: 18 June 2020Accepted: 07 January 2021Published online: 15 April 2021Keywordsinterface conditions, homogenization, boundary layer, porous medium, free flowAMS Subject Headings35Q35, 76D07, 76M10, 76M50, 76S05Publication DataISSN (print): 1540-3459ISSN (online): 1540-3467Publisher: Society for Industrial and Applied MathematicsCODEN: mmsubt

10.1137/20m1346638 article EN Multiscale Modeling and Simulation 2021-01-01

Abstract Physically consistent coupling conditions at the fluid–porous interface with correctly determined effective parameters are necessary for accurate modeling and simulation of various applications. To describe single-fluid-phase flows in coupled free-flow porous-medium systems, Stokes/Darcy equations typically used together conservation mass across interface, balance normal forces Beavers–Joseph condition on tangential velocity. The latter is suitable parallel to but not applicable...

10.1007/s11242-023-01919-3 article EN cc-by Transport in Porous Media 2023-03-13

Abstract Existing model validation studies in geoscience often disregard or partly account for uncertainties observations, choices, and input parameters. In this work, we develop a statistical framework that incorporates probabilistic modeling technique using fully Bayesian approach to perform quantitative uncertainty-aware validation. A perspective on task yields an optimal bias-variance trade-off against the reference data. It provides integrative metric parameter conceptual uncertainty....

10.1007/s10596-023-10228-z article EN cc-by Computational Geosciences 2023-07-13

Fluid flows in coupled systems consisting of a free-flow region and the adjacent porous medium appear variety environmental settings industrial applications. In many applications, fluid flow is non-parallel to fluid–porous interface that requires generalisation Beavers–Joseph coupling condition typically used for Stokes–Darcy problem. Generalised conditions valid arbitrary directions are recently derived using theory homogenisation boundary layers. The aim this work mathematical analysis...

10.1051/m2an/2022025 article EN cc-by ESAIM. Mathematical modelling and numerical analysis 2022-03-01

Boundary conditions at the interface between free-flow region and adjacent porous medium is a key issue for physically consistent modeling accurate numerical simulation of flow transport processes in coupled systems due to driven nature such processes. Interface available literature have several weak points: most them are suitable only flows parallel fluid-porous interface, some restricted specific boundary value problems, others contain unknown model parameters which still need be...

10.48550/arxiv.2006.12096 preprint EN other-oa arXiv (Cornell University) 2020-01-01

Existing model validation studies in geoscience often disregard or partly account for uncertainties observations, choices, and input parameters. In this work, we develop a statistical framework that incorporates probabilistic modeling technique using fully Bayesian approach to perform quantitative uncertainty-aware validation. A perspective on task yields an optimal bias-variance trade-off against the reference data. It provides integrative metric parameter conceptual uncertainty....

10.48550/arxiv.2106.13639 preprint EN other-oa arXiv (Cornell University) 2021-01-01

The correct choice of interface conditions and effective parameters for coupled macroscale free-flow porous-medium models is crucial a complete mathematical description the problem under consideration accurate numerical simulation applications. We consider single-fluid-phase systems described by Stokes-Darcy model. Different sets coupling this model are available. However, these often arbitrary. use large scale lattice Boltzmann simulations to validate comparison against pore-scale resolved...

10.48550/arxiv.1906.06884 preprint EN other-oa arXiv (Cornell University) 2019-01-01

Physically consistent coupling conditions at the fluid-porous interface with correctly determined effective parameters are necessary for accurate modeling and simulation of various applications. To describe single-fluid-phase flows in coupled free-flow porous-medium systems, Stokes/Darcy equations typically used together conservation mass across interface, balance normal forces Beavers-Joseph condition on tangential velocity. The latter is suitable parallel to but not applicable arbitrary...

10.48550/arxiv.2106.15556 preprint EN other-oa arXiv (Cornell University) 2021-01-01

Fluid flows in coupled systems consisting of a free-flow region and the adjacent porous medium appear variety environmental settings industrial applications. In many applications, fluid flow is non-parallel to fluid-porous interface that requires generalisation Beavers-Joseph coupling condition typically used for Stokes-Darcy problem. Generalised conditions valid arbitrary directions are recently derived using theory homogenisation boundary layers. The aim this work mathematical analysis...

10.48550/arxiv.2104.02339 preprint EN other-oa arXiv (Cornell University) 2021-01-01
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