A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY

The knowledge of solute transport process in the porous media has an important role for addressing chemical pollution, loss of nutrients, groundwater contaminating rate and drainage water quality. The aim of this paper was to review the hydrodynamic dispersivity parameter and the models of dispersio...

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Main Author: Fereshte Haghighi Fashi
Format: Article
Language:English
Published: AcademicPres 2015-12-01
Series:Agricultura
Online Access:http://journals.usamvcluj.ro/index.php/agricultura/article/view/11791
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spelling doaj-9e6ce4d513db42089f0faad101a45f212021-09-02T02:29:23ZengAcademicPresAgricultura1221-53172015-12-01953-410.15835/arspa.v95i3-4.117919635A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITYFereshte Haghighi Fashi0University of Tehran, Tehran, IranThe knowledge of solute transport process in the porous media has an important role for addressing chemical pollution, loss of nutrients, groundwater contaminating rate and drainage water quality. The aim of this paper was to review the hydrodynamic dispersivity parameter and the models of dispersion - mass and stochastic to evaluate the solute transport process in soils. Solute transport models, convective - dispersive Equation (CDE) and convective lognormal transfer (CLT) are fitted to experimental breakthrough curves (BTC’s) and solute transport parameters are estimated. It should be investigated which of the CDE or CLT model explain the BTCs more reliably. The review indicates that the soil physical properties and experiment conditions can determine the appropriate model that characterizes the BTCs. The travel time distribution and the variance of solute molecule velocities vary with flow rate. Mohammadi and Vanclooster (2012) indicated that the mean solute travel time, μt, increases partially with the travel distance and decreases with the flow rate. The review shows that the mean travel time distribution depends on the flow rate. Generally, well - controlled solute transport experiments on soils are essential to the knowledge of the solute transport processes and parameters for different flow rates and soil types.http://journals.usamvcluj.ro/index.php/agricultura/article/view/11791
collection DOAJ
language English
format Article
sources DOAJ
author Fereshte Haghighi Fashi
spellingShingle Fereshte Haghighi Fashi
A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
Agricultura
author_facet Fereshte Haghighi Fashi
author_sort Fereshte Haghighi Fashi
title A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
title_short A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
title_full A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
title_fullStr A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
title_full_unstemmed A REVIEW OF SOLUTE TRANSPORT MODELING IN SOILS AND HYDRODYNAMIC DISPERSIVITY
title_sort review of solute transport modeling in soils and hydrodynamic dispersivity
publisher AcademicPres
series Agricultura
issn 1221-5317
publishDate 2015-12-01
description The knowledge of solute transport process in the porous media has an important role for addressing chemical pollution, loss of nutrients, groundwater contaminating rate and drainage water quality. The aim of this paper was to review the hydrodynamic dispersivity parameter and the models of dispersion - mass and stochastic to evaluate the solute transport process in soils. Solute transport models, convective - dispersive Equation (CDE) and convective lognormal transfer (CLT) are fitted to experimental breakthrough curves (BTC’s) and solute transport parameters are estimated. It should be investigated which of the CDE or CLT model explain the BTCs more reliably. The review indicates that the soil physical properties and experiment conditions can determine the appropriate model that characterizes the BTCs. The travel time distribution and the variance of solute molecule velocities vary with flow rate. Mohammadi and Vanclooster (2012) indicated that the mean solute travel time, μt, increases partially with the travel distance and decreases with the flow rate. The review shows that the mean travel time distribution depends on the flow rate. Generally, well - controlled solute transport experiments on soils are essential to the knowledge of the solute transport processes and parameters for different flow rates and soil types.
url http://journals.usamvcluj.ro/index.php/agricultura/article/view/11791
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