Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams

While flowing through porous medium, ground water flow dissolves minerals thereby in creasing medium porosity and ultimately permeability. Reactive fluid flows preferentially into highly permeable zones, which are therefore dissolved most rapidly, producing a further preferential permeability enhanc...

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Main Authors: Jui-Sheng Chen, Yuan-Yao Chang, Chen-Wuing Liu
Format: Article
Language:English
Published: Chinese Geoscience Union 2009-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v206p839.pdf
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spelling doaj-087244dc0eaa486fac7361e8bb5a6e102020-11-24T21:29:02ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802009-01-0120683910.3319/TAO.2008.11.07.01(Hy)883Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior DiagramsJui-Sheng ChenYuan-Yao ChangChen-Wuing LiuWhile flowing through porous medium, ground water flow dissolves minerals thereby in creasing medium porosity and ultimately permeability. Reactive fluid flows preferentially into highly permeable zones, which are therefore dissolved most rapidly, producing a further preferential permeability enhancement. Accordingly, slight non-uniformities present in porous medium can be amplified and lead to fingering reaction fronts. The objective of this study is to investigate dissolution-induced porosity changes on reaction front morphology in homogeneous porous medium with two non-uniformities. Four controlling parameters, including up stream pressure gradient, reaction rate constant, non-uniformities spacing and non-uniformity strength ratio are comprehensively considered. By using a modified version of the numerical code, NSPCRT, to conduct a series of numerical simulations, front behavior diagrams are constructed to illustrate the morphologies of reaction fronts under various combinations of these four factors. Simulation results indicate that the two non-uniformities are inhibited into a planar front under low up stream pressure gradient, merge into a single-fingering front under inter mediate up stream pressure gradient, or grow into a double-fingers front under high up stream pressure gradient. More over, the two non-uniformities tend to develop intoadouble-fingering front as the non-uniformity strength ratio in creases from 0.2 to 1.0, and merge into a single-fingering front while the non-uniformity strength ratio in creases from 1.0 to 1.8. When the reaction rate constant is small, the two non-uniformities merge into a single front. Reaction rate constant significantly affects front advancing velocity. The front advancing velocity decreases with the reaction rate constant. Based on these results, front behavior diagrams which de fine the morphologies of the reaction fronts for these four parameters are constructed. Moreover, non-uniformity strength ratio and reaction rate constant are identified as two important factors that govern the interaction of dissolution and solute transport in groundwater systems. http://tao.cgu.org.tw/images/attachments/v206p839.pdf PorosityKinetic dissolution reactionNon-uni formity strength ratioReaction ratecon stantFront behavior diagram
collection DOAJ
language English
format Article
sources DOAJ
author Jui-Sheng Chen
Yuan-Yao Chang
Chen-Wuing Liu
spellingShingle Jui-Sheng Chen
Yuan-Yao Chang
Chen-Wuing Liu
Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
Terrestrial, Atmospheric and Oceanic Sciences
Porosity
Kinetic dissolution reaction
Non-uni formity strength ratio
Reaction ratecon stant
Front behavior diagram
author_facet Jui-Sheng Chen
Yuan-Yao Chang
Chen-Wuing Liu
author_sort Jui-Sheng Chen
title Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
title_short Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
title_full Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
title_fullStr Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
title_full_unstemmed Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams
title_sort evaluation of front morphological development of reactive solute transport using behavior diagrams
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2009-01-01
description While flowing through porous medium, ground water flow dissolves minerals thereby in creasing medium porosity and ultimately permeability. Reactive fluid flows preferentially into highly permeable zones, which are therefore dissolved most rapidly, producing a further preferential permeability enhancement. Accordingly, slight non-uniformities present in porous medium can be amplified and lead to fingering reaction fronts. The objective of this study is to investigate dissolution-induced porosity changes on reaction front morphology in homogeneous porous medium with two non-uniformities. Four controlling parameters, including up stream pressure gradient, reaction rate constant, non-uniformities spacing and non-uniformity strength ratio are comprehensively considered. By using a modified version of the numerical code, NSPCRT, to conduct a series of numerical simulations, front behavior diagrams are constructed to illustrate the morphologies of reaction fronts under various combinations of these four factors. Simulation results indicate that the two non-uniformities are inhibited into a planar front under low up stream pressure gradient, merge into a single-fingering front under inter mediate up stream pressure gradient, or grow into a double-fingers front under high up stream pressure gradient. More over, the two non-uniformities tend to develop intoadouble-fingering front as the non-uniformity strength ratio in creases from 0.2 to 1.0, and merge into a single-fingering front while the non-uniformity strength ratio in creases from 1.0 to 1.8. When the reaction rate constant is small, the two non-uniformities merge into a single front. Reaction rate constant significantly affects front advancing velocity. The front advancing velocity decreases with the reaction rate constant. Based on these results, front behavior diagrams which de fine the morphologies of the reaction fronts for these four parameters are constructed. Moreover, non-uniformity strength ratio and reaction rate constant are identified as two important factors that govern the interaction of dissolution and solute transport in groundwater systems.
topic Porosity
Kinetic dissolution reaction
Non-uni formity strength ratio
Reaction ratecon stant
Front behavior diagram
url http://tao.cgu.org.tw/images/attachments/v206p839.pdf
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