Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method

This study investigates the numerical simulation of fluid flow in a flat layer near a porous bottom layer in gravity field. The porosity distribution along the bottom is assumed to be homogeneous. The upper part of the layer is free of the porous medium, while the porosity is in the lower part. This...

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Main Authors: Volodin Ivan, Alabuzhev Alexey
Format: Article
Language:English
Published: EDP Sciences 2024-01-01
Series:BIO Web of Conferences
Online Access:https://www.bio-conferences.org/articles/bioconf/pdf/2024/64/bioconf_ForestryForum2024_02019.pdf
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author Volodin Ivan
Alabuzhev Alexey
author_facet Volodin Ivan
Alabuzhev Alexey
author_sort Volodin Ivan
collection DOAJ
description This study investigates the numerical simulation of fluid flow in a flat layer near a porous bottom layer in gravity field. The porosity distribution along the bottom is assumed to be homogeneous. The upper part of the layer is free of the porous medium, while the porosity is in the lower part. This task describes, for example, the flow near bottom vegetation. The problem is solved using the Lattice Boltzmann Method. The porous medium is simulated by the representative elementary volume (REV) method. The system is studied in an isothermal formulation with different porosity and permeability coefficients.
format Article
id doaj-art-8be52be18fec4872ae13832a34f3c3d8
institution OA Journals
issn 2117-4458
language English
publishDate 2024-01-01
publisher EDP Sciences
record_format Article
series BIO Web of Conferences
spelling doaj-art-8be52be18fec4872ae13832a34f3c3d82025-08-20T01:59:26ZengEDP SciencesBIO Web of Conferences2117-44582024-01-011450201910.1051/bioconf/202414502019bioconf_ForestryForum2024_02019Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann MethodVolodin Ivan0Alabuzhev Alexey1Institute of Continuous Media Mechanics UB RASInstitute of Continuous Media Mechanics UB RASThis study investigates the numerical simulation of fluid flow in a flat layer near a porous bottom layer in gravity field. The porosity distribution along the bottom is assumed to be homogeneous. The upper part of the layer is free of the porous medium, while the porosity is in the lower part. This task describes, for example, the flow near bottom vegetation. The problem is solved using the Lattice Boltzmann Method. The porous medium is simulated by the representative elementary volume (REV) method. The system is studied in an isothermal formulation with different porosity and permeability coefficients.https://www.bio-conferences.org/articles/bioconf/pdf/2024/64/bioconf_ForestryForum2024_02019.pdf
spellingShingle Volodin Ivan
Alabuzhev Alexey
Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
BIO Web of Conferences
title Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
title_full Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
title_fullStr Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
title_full_unstemmed Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
title_short Simulation of flow near bottom vegetation in two layers channel by the Lattice Boltzmann Method
title_sort simulation of flow near bottom vegetation in two layers channel by the lattice boltzmann method
url https://www.bio-conferences.org/articles/bioconf/pdf/2024/64/bioconf_ForestryForum2024_02019.pdf
work_keys_str_mv AT volodinivan simulationofflownearbottomvegetationintwolayerschannelbythelatticeboltzmannmethod
AT alabuzhevalexey simulationofflownearbottomvegetationintwolayerschannelbythelatticeboltzmannmethod