An open source massively parallel solver for Richards equation: mechanistic modelling of water fluxes at the watershed scale

DOI10.1016/j.cpc.2014.08.004zbMath1360.76008arXiv1809.10895OpenAlexW2117855192WikidataQ115045426 ScholiaQ115045426MaRDI QIDQ525749

Yong-Cai Geng, Sumit K. Garg

Publication date: 5 May 2017

Published in: Computer Physics Communications (Search for Journal in Brave)

Full work available at URL: https://arxiv.org/abs/1809.10895

zbMATH Keywords

porous mediaRichards equationOpenFOAM\(^{\circledR}\)massively parallel computationtransfers in soilsvariably saturated flow

Mathematics Subject Classification ID

PDEs in connection with fluid mechanics (35Q35) Flows in porous media; filtration; seepage (76S05) Parallel numerical computation (65Y05) Software, source code, etc. for problems pertaining to fluid mechanics (76-04)

Related Items (6)

porousMultiphaseFoam v2107: an open-source tool for modeling saturated/unsaturated water flows and solute transfers at watershed scale ⋮ A novel vertex-centered finite volume method for solving Richards' equation and its adaptation to local mesh refinement ⋮ Multiphase flow modeling in multiscale porous media: an open-source micro-continuum approach ⋮ Enhancing speed and scalability of the ParFlow simulation code ⋮ Pore-scale modelling of multiphase reactive flow: application to mineral dissolution with production of ⋮ Multiscale simulations for multi-continuum Richards equations

Uses Software

• OpenFOAM
• RichardsFOAM
• RichardsFoam2
• BIGFLOW
• FEMWATER
• TOUGH

Cites Work

• Unnamed Item
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• The finite volume method for Richards equation
• Hydraulic conductivity estimation in partially saturated soils using the adjoint method
• An edge-based finite volume scheme for saturated--unsaturated groundwater flow
• Locally conservative, stabilized finite element methods for variably saturated flow
• CAPILLARY CONDUCTION OF LIQUIDS THROUGH POROUS MEDIUMS
• Load balancing fictions, falsehoods and fallacies

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