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ELYES AHMED
ELYES AHMED
SINTEF Digital, Oslo, Norway
Verified email at sintef.no - Homepage
Title
Cited by
Cited by
Year
A reduced fracture model for two-phase flow with different rock types
E Ahmed, J Jaffré, JE Roberts
Mathematics and Computers in Simulation 137, 49-70, 2017
632017
Adaptive asynchronous time-stepping, stopping criteria, and a posteriori error estimates for fixed-stress iterative schemes for coupled poromechanics problems
E Ahmed, JM Nordbotten, FA Radu
Journal of Computational and Applied Mathematics 364, 112312, 2020
382020
Monolithic and splitting solution schemes for fully coupled quasi-static thermo-poroelasticity with nonlinear convective transport
MK Brun, E Ahmed, I Berre, JM Nordbotten, FA Radu
Computers & Mathematics with Applications 80 (8), 1964-1984, 2020
362020
Adaptive poromechanics computations based on a posteriori error estimates for fully mixed formulations of Biot’s consolidation model
E Ahmed, FA Radu, JM Nordbotten
Computer Methods in Applied Mechanics and Engineering 347, 264-294, 2019
312019
Well-posedness of the fully coupled quasi-static thermo-poroelastic equations with nonlinear convective transport
MK Brun, E Ahmed, JM Nordbotten, FA Radu
Journal of Mathematical Analysis and Applications 471 (1-2), 239-266, 2019
272019
A posteriori error estimates and stopping criteria for space-time domain decomposition for two-phase flow between different rock types
E Ahmed, S Ali Hassan, C Japhet, M Kern, M Vohralík
The SMAI journal of computational mathematics 5, 195-227, 2019
272019
Space-time domain decomposition for two-phase flow between different rock types
E Ahmed, C Japhet, M Kern
152020
A multiscale flux basis for mortar mixed discretizations of reduced Darcy–Forchheimer fracture models
E Ahmed, A Fumagalli, A Budiša
Computer Methods in Applied Mechanics and Engineering 354, 16-36, 2019
132019
Splitting-based domain decomposition methods for two-phase flow with different rock types
E Ahmed
Advances in water resources 134, 103431, 2019
102019
Robust linear domain decomposition schemes for reduced nonlinear fracture flow models
E Ahmed, A Fumagalli, A Budisa, E Keilegavlen, JM Nordbotten, FA Radu
SIAM Journal on Numerical Analysis 59 (1), 583-612, 2021
82021
A posteriori error estimates for hierarchical mixed-dimensional elliptic equations
J Varela, E Ahmed, E Keilegavlen, JM Nordbotten, FA Radu
Journal of Numerical Mathematics 31 (4), 247-280, 2023
62023
A finite volume Schwarz algorithm for two-phase immiscible flow with different rock types
E Ahmed, C Japhet, M Kern
preparation, 0
5
Global–in–Time Domain Decomposition for a Nonlinear Diffusion Problem
E Ahmed, C Japhet, M Kern
Domain Decomposition Methods in Science and Engineering XXV 25, 202-209, 2020
42020
Modeling the process of speciation using a multiscale framework including a posteriori error estimates
MK Brun, E Ahmed, JM Nordbotten, N Chr
SIAM Journal on Applied Mathematics 82 (2), 450-475, 2022
32022
The sub-Cauchy–Stokes problem: Solvability issues and Lagrange multiplier methods with artificial boundary conditions
E Ahmed, AB Abda
Journal of Computational and Applied Mathematics 338, 258-279, 2018
32018
A posteriori error estimates and adaptivity for fully mixed finite element discretizations for Biot’s consolidation model
E Ahmed, FA Radu, JM Nordbotten
working paper or preprint, 2018
32018
Adaptive timestepping, linearization, and a posteriori error control for multiphase flow of immiscible fluids in porous media with wells
E Ahmed, Ø Klemetsdal, X Raynaud, O Møyner, HM Nilsen
SPE Journal 28 (02), 554-574, 2023
22023
A 3-D reduced fracture model for two-phase flow in porous media with a global pressure formulation
A Elyes, J Jérôme, JE Roberts
MAMERN VI, Pau, France, 2015
22015
Adaptive Time Stepping, Linearization and a Posteriori Error Control for Multiphase Flow with Wells
E Ahmed, Ø Klemetsdal, X Raynaud, O Møyner, HM Nilsen
SPE Reservoir Simulation Conference?, D011S009R004, 2021
12021
Efficient Adaptive Solvers for Doubly Degenerate Elliptic Equations using A Posteriori Error Estimates
E Ahmed, S Amdouni
2024
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