Folgen
Hamdi Tchelepi
Hamdi Tchelepi
Professor of Energy Science and Engineering, Stanford University
Bestätigte E-Mail-Adresse bei stanford.edu - Startseite
Titel
Zitiert von
Zitiert von
Jahr
Multi-scale finite-volume method for elliptic problems in subsurface flow simulation
P Jenny, SH Lee, HA Tchelepi
Journal of computational physics 187 (1), 47-67, 2003
9152003
Onset of convection in a gravitationally unstable diffusive boundary layer in porous media
A Riaz, M Hesse, HA Tchelepi, FM Orr
Journal of Fluid Mechanics 548, 87-111, 2006
8572006
Stability and convergence of sequential methods for coupled flow and geomechanics: Fixed-stress and fixed-strain splits
J Kim, HA Tchelepi, R Juanes
Computer Methods in Applied Mechanics and Engineering 200 (13-16), 1591-1606, 2011
5202011
Physics-informed machine learning: case studies for weather and climate modelling
K Kashinath, M Mustafa, A Albert, JL Wu, C Jiang, S Esmaeilzadeh, ...
Philosophical Transactions of the Royal Society A 379 (2194), 20200093, 2021
5052021
Stability, accuracy, and efficiency of sequential methods for coupled flow and geomechanics
J Kim, HA Tchelepi, R Juanes
SPE Journal 16 (02), 249-262, 2011
4602011
Convective dissolution of carbon dioxide in saline aquifers
JA Neufeld, MA Hesse, A Riaz, MA Hallworth, HA Tchelepi, HE Huppert
Geophysical research letters 37 (22), 2010
4032010
Gravity currents with residual trapping
MA Hesse, FM Orr, HA Tchelepi
Journal of Fluid Mechanics 611, 35-60, 2008
3702008
Adaptive multiscale finite-volume method for multiphase flow and transport in porous media
P Jenny, SH Lee, HA Tchelepi
Multiscale Modeling & Simulation 3 (1), 50-64, 2005
3372005
Adaptive fully implicit multi-scale finite-volume method for multi-phase flow and transport in heterogeneous porous media
P Jenny, SH Lee, HA Tchelepi
Journal of Computational Physics 217 (2), 627-641, 2006
2922006
Limitations of physics informed machine learning for nonlinear two-phase transport in porous media
O Fuks, HA Tchelepi
Journal of Machine Learning for Modeling and Computing 1 (1), 2020
2662020
Stability and convergence of sequential methods for coupled flow and geomechanics: Drained and undrained splits
J Kim, HA Tchelepi, R Juanes
Computer Methods in Applied Mechanics and Engineering 200 (23-24), 2094-2116, 2011
2572011
Parallel scalable unstructured CPR-type linear solver for reservoir simulation
H Cao, HA Tchelepi, J Wallis, H Yardumian
SPE Annual Technical Conference and Exhibition?, SPE-96809-MS, 2005
2412005
Discrete fracture model for coupled flow and geomechanics
TT Garipov, M Karimi-Fard, HA Tchelepi
Computational Geosciences 20, 149-160, 2016
2302016
Mineral dissolution and wormholing from a pore-scale perspective
C Soulaine, S Roman, A Kovscek, HA Tchelepi
Journal of Fluid Mechanics 827, 457-483, 2017
2252017
Comparison of nonlinear formulations for two-phase multi-component EoS based simulation
DV Voskov, HA Tchelepi
Journal of Petroleum Science and Engineering 82, 101-111, 2012
2122012
Block-partitioned solvers for coupled poromechanics: A unified framework
JA White, N Castelletto, HA Tchelepi
Computer Methods in Applied Mechanics and Engineering 303, 55-74, 2016
1902016
Accuracy and convergence properties of the fixed‐stress iterative solution of two‐way coupled poromechanics
N Castelletto, JA White, HA Tchelepi
International Journal for Numerical and Analytical Methods in Geomechanics …, 2015
1812015
Interaction of viscous fingering, permeability heterogeneity, and gravity segregation in three dimensions
HA Tchelepi, FM Orr
SPE Reservoir Engineering 9 (04), 266-271, 1994
181*1994
Multiscale finite-volume formulation for multiphase flow in porous media: black oil formulation of compressible, three-phase flow with gravity
SH Lee, C Wolfsteiner, HA Tchelepi
Computational Geosciences 12, 351-366, 2008
1802008
The impact of sub-resolution porosity of X-ray microtomography images on the permeability
C Soulaine, F Gjetvaj, C Garing, S Roman, A Russian, P Gouze, ...
Transport in porous media 113, 227-243, 2016
1792016
Das System kann den Vorgang jetzt nicht ausführen. Versuchen Sie es später erneut.
Artikel 1–20