Influence of source thickness on steady-state plume length

The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. (2005, 2011) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were o...

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Published inEnvironmental earth sciences Vol. 71; no. 2; pp. 959 - 964
Main Authors Yadav, P. K, Liedl, R, Dietrich, P
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer-Verlag 01.01.2014
Springer Berlin Heidelberg
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Abstract The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. (2005, 2011) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were obtained: first, the modified expressions overestimate the plume length only up to a factor of 2 when the source thickness (M ₛ ) is at least 50 % of the aquifer depth (M). Second, overestimates do not exceed plume length by a factor of 10 (2D scenario) or 5 (3D scenario) for 25 % < M ₛ /M < 50 %. Third, numerical techniques are recommended for M ₛ < 25 %. In addition, it was observed that the degradation from the top dominates for M ₛ /M > 50 %. As far as the numerical experiments are concerned, it is important to note that the employed finite element approach was applied to the transformed transport equation provided in both Liedl et al. works. This transformation, which can also be applied to more complex scenarios than those studied here, eliminates reaction terms from the model equations and therefore largely facilitates numerical computations.
AbstractList The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. ( 2005 , 2011 ) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were obtained: first, the modified expressions overestimate the plume length only up to a factor of 2 when the source thickness ( M s ) is at least 50 % of the aquifer depth ( M ). Second, overestimates do not exceed plume length by a factor of 10 (2D scenario) or 5 (3D scenario) for 25 % <  M s / M  < 50 %. Third, numerical techniques are recommended for M s  < 25 %. In addition, it was observed that the degradation from the top dominates for M s / M  > 50 %. As far as the numerical experiments are concerned, it is important to note that the employed finite element approach was applied to the transformed transport equation provided in both Liedl et al. works. This transformation, which can also be applied to more complex scenarios than those studied here, eliminates reaction terms from the model equations and therefore largely facilitates numerical computations.
The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. (2005, 2011) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were obtained: first, the modified expressions overestimate the plume length only up to a factor of 2 when the source thickness (M s ) is at least 50 % of the aquifer depth (M). Second, overestimates do not exceed plume length by a factor of 10 (2D scenario) or 5 (3D scenario) for 25 % < M s /M < 50 %. Third, numerical techniques are recommended for M s < 25 %. In addition, it was observed that the degradation from the top dominates for M s /M > 50 %. As far as the numerical experiments are concerned, it is important to note that the employed finite element approach was applied to the transformed transport equation provided in both Liedl et al. works. This transformation, which can also be applied to more complex scenarios than those studied here, eliminates reaction terms from the model equations and therefore largely facilitates numerical computations.
Issue Title: Thematic Issue: Besancon - Karst aquifers The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. ( 2005 , 2011 ) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were obtained: first, the modified expressions overestimate the plume length only up to a factor of 2 when the source thickness (M ^sub s^) is at least 50 % of the aquifer depth (M). Second, overestimates do not exceed plume length by a factor of 10 (2D scenario) or 5 (3D scenario) for 25 % < M ^sub s^/M < 50 %. Third, numerical techniques are recommended for M ^sub s^ < 25 %. In addition, it was observed that the degradation from the top dominates for M ^sub s^/M > 50 %. As far as the numerical experiments are concerned, it is important to note that the employed finite element approach was applied to the transformed transport equation provided in both Liedl et al. works. This transformation, which can also be applied to more complex scenarios than those studied here, eliminates reaction terms from the model equations and therefore largely facilitates numerical computations.[PUBLICATION ABSTRACT]
The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. (2005, 2011) for 2D and 3D scenarios. For comparison, 2D and 3D numerical experiments were performed, and the following three important conclusions were obtained: first, the modified expressions overestimate the plume length only up to a factor of 2 when the source thickness (M ₛ ) is at least 50 % of the aquifer depth (M). Second, overestimates do not exceed plume length by a factor of 10 (2D scenario) or 5 (3D scenario) for 25 % < M ₛ /M < 50 %. Third, numerical techniques are recommended for M ₛ < 25 %. In addition, it was observed that the degradation from the top dominates for M ₛ /M > 50 %. As far as the numerical experiments are concerned, it is important to note that the employed finite element approach was applied to the transformed transport equation provided in both Liedl et al. works. This transformation, which can also be applied to more complex scenarios than those studied here, eliminates reaction terms from the model equations and therefore largely facilitates numerical computations.
Author Yadav, P. K
Dietrich, P
Liedl, R
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Issue 2
Keywords Numerical modeling
Analytical models
Plume length
experimental studies
thickness
plumes
ground water
degradation
transport
finite element analysis
depth
aquifers
numerical models
three-dimensional models
transformations
two-dimensional models
Language English
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PublicationTitle Environmental earth sciences
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Snippet The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. (2005, 2011)...
The impact of source thickness on steady-state plume length is studied using modifications of the analytical expressions provided in Liedl et al. ( 2005 , 2011...
Issue Title: Thematic Issue: Besancon - Karst aquifers The impact of source thickness on steady-state plume length is studied using modifications of the...
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SubjectTerms Aquifers
Biogeosciences
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Environmental Science and Engineering
equations
Exact sciences and technology
Geochemistry
Geology
Groundwater pollution
Hydrogeology
Hydrology. Hydrogeology
Hydrology/Water Resources
Karst
Mathematical analysis
Mathematical models
Original Article
Plumes
pollution
Pollution, environment geology
Terrestrial Pollution
Three dimensional
Transformations
Transport equations
Two dimensional
Water resources management
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Title Influence of source thickness on steady-state plume length
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