Particulate transport through heterogeneous porous media; numerical studies using finite element method

The complexity of natural systems often prohibits our understanding of governing principles of the systems. The prediction of flow and solute transport through large-scale geological systems is challenging, since accurate predictions involves a detailed characterization of the spatial distribution o...

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Main Author: M Ilie
Format: Article
Language:English
Published: Multi-Science Publishing 2016-09-01
Series:International Journal of Multiphysics
Online Access:http://journal.multiphysics.org/index.php/IJM/article/view/238
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spelling doaj-62ad4cbcffda40f689febd663073c5d62020-11-24T23:01:59ZengMulti-Science PublishingInternational Journal of Multiphysics1750-95482048-39612016-09-017310.1260/1750-9548.7.3.245250Particulate transport through heterogeneous porous media; numerical studies using finite element methodM Ilie0Sat Tomsani, Com. Costestii din Vale, Jud. Dambovita RomaniaThe complexity of natural systems often prohibits our understanding of governing principles of the systems. The prediction of flow and solute transport through large-scale geological systems is challenging, since accurate predictions involves a detailed characterization of the spatial distribution of hydrologic parameter values. For simplicity reasons, most of the past studies of groundwater flow and solute transport assumed homogeneous aquifers. Numerical methods of estimating hydrologic properties of aquifers used the homogeneity assumption because of mathematical challenges associated with the heterogeneity of aquifers. In the present work we investigate the transport processes in watersheds using a two-dimensional model for flow and particulate transport in the subsurface system. The study reveals that the particle dispersion depends strongly on the heterogeneity of the aquifer. Thus, the particles exhibit a slower speed in the regions of low conductivity. Moreover, the particles exhibit a preferential path, following the path of minimum resistance.http://journal.multiphysics.org/index.php/IJM/article/view/238
collection DOAJ
language English
format Article
sources DOAJ
author M Ilie
spellingShingle M Ilie
Particulate transport through heterogeneous porous media; numerical studies using finite element method
International Journal of Multiphysics
author_facet M Ilie
author_sort M Ilie
title Particulate transport through heterogeneous porous media; numerical studies using finite element method
title_short Particulate transport through heterogeneous porous media; numerical studies using finite element method
title_full Particulate transport through heterogeneous porous media; numerical studies using finite element method
title_fullStr Particulate transport through heterogeneous porous media; numerical studies using finite element method
title_full_unstemmed Particulate transport through heterogeneous porous media; numerical studies using finite element method
title_sort particulate transport through heterogeneous porous media; numerical studies using finite element method
publisher Multi-Science Publishing
series International Journal of Multiphysics
issn 1750-9548
2048-3961
publishDate 2016-09-01
description The complexity of natural systems often prohibits our understanding of governing principles of the systems. The prediction of flow and solute transport through large-scale geological systems is challenging, since accurate predictions involves a detailed characterization of the spatial distribution of hydrologic parameter values. For simplicity reasons, most of the past studies of groundwater flow and solute transport assumed homogeneous aquifers. Numerical methods of estimating hydrologic properties of aquifers used the homogeneity assumption because of mathematical challenges associated with the heterogeneity of aquifers. In the present work we investigate the transport processes in watersheds using a two-dimensional model for flow and particulate transport in the subsurface system. The study reveals that the particle dispersion depends strongly on the heterogeneity of the aquifer. Thus, the particles exhibit a slower speed in the regions of low conductivity. Moreover, the particles exhibit a preferential path, following the path of minimum resistance.
url http://journal.multiphysics.org/index.php/IJM/article/view/238
work_keys_str_mv AT milie particulatetransportthroughheterogeneousporousmedianumericalstudiesusingfiniteelementmethod
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