Influence of layering on the formation and growth of solution pipes

In karst systems, hydraulic conduits called solution pipes (or wormholes) are formed as a result of the dissolution of limestone rocks by the water surcharged with CO2. The solution pipes are the end result of a positive feedback between spatial variations in porosity in the rock matrix and the loca...

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Main Authors: Karine ePetrus, Piotr eSzymczak
Format: Article
Language:English
Published: Frontiers Media S.A. 2016-01-01
Series:Frontiers in Physics
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fphy.2015.00092/full
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spelling doaj-5ad89796f5774ed4a1ed0af14e727bdf2020-11-24T23:43:29ZengFrontiers Media S.A.Frontiers in Physics2296-424X2016-01-01310.3389/fphy.2015.00092159289Influence of layering on the formation and growth of solution pipesKarine ePetrus0Piotr eSzymczak1University of WarsawUniversity of WarsawIn karst systems, hydraulic conduits called solution pipes (or wormholes) are formed as a result of the dissolution of limestone rocks by the water surcharged with CO2. The solution pipes are the end result of a positive feedback between spatial variations in porosity in the rock matrix and the local dissolution rate. Here, we investigate numerically the effect of rock stratification on the solution pipe growth, using a simple model system with a number of horizontal layers, which are less porous than the rest of the matrix. Stratification is shown to affect the resulting piping patterns in a variety of ways. First of all, it enhances the competition between the pipes, impeding the growth of the shorter ones and enhancing the flow in the longer ones, which therefore grow longer. This is reflected in the change of the pipe length distribution, which becomes steeper as the porosity contrast between the layers is increased. Additionally, stratification affects the shapes of individual solution pipes, with characteristic widening of the profiles in between the layers and narrowing within the layers. These results are in qualitative agreement with the piping morphologies observed in nature.http://journal.frontiersin.org/Journal/10.3389/fphy.2015.00092/fullkarstdissolutionPorous mediumReactive flowSolution pipes
collection DOAJ
language English
format Article
sources DOAJ
author Karine ePetrus
Piotr eSzymczak
spellingShingle Karine ePetrus
Piotr eSzymczak
Influence of layering on the formation and growth of solution pipes
Frontiers in Physics
karst
dissolution
Porous medium
Reactive flow
Solution pipes
author_facet Karine ePetrus
Piotr eSzymczak
author_sort Karine ePetrus
title Influence of layering on the formation and growth of solution pipes
title_short Influence of layering on the formation and growth of solution pipes
title_full Influence of layering on the formation and growth of solution pipes
title_fullStr Influence of layering on the formation and growth of solution pipes
title_full_unstemmed Influence of layering on the formation and growth of solution pipes
title_sort influence of layering on the formation and growth of solution pipes
publisher Frontiers Media S.A.
series Frontiers in Physics
issn 2296-424X
publishDate 2016-01-01
description In karst systems, hydraulic conduits called solution pipes (or wormholes) are formed as a result of the dissolution of limestone rocks by the water surcharged with CO2. The solution pipes are the end result of a positive feedback between spatial variations in porosity in the rock matrix and the local dissolution rate. Here, we investigate numerically the effect of rock stratification on the solution pipe growth, using a simple model system with a number of horizontal layers, which are less porous than the rest of the matrix. Stratification is shown to affect the resulting piping patterns in a variety of ways. First of all, it enhances the competition between the pipes, impeding the growth of the shorter ones and enhancing the flow in the longer ones, which therefore grow longer. This is reflected in the change of the pipe length distribution, which becomes steeper as the porosity contrast between the layers is increased. Additionally, stratification affects the shapes of individual solution pipes, with characteristic widening of the profiles in between the layers and narrowing within the layers. These results are in qualitative agreement with the piping morphologies observed in nature.
topic karst
dissolution
Porous medium
Reactive flow
Solution pipes
url http://journal.frontiersin.org/Journal/10.3389/fphy.2015.00092/full
work_keys_str_mv AT karineepetrus influenceoflayeringontheformationandgrowthofsolutionpipes
AT piotreszymczak influenceoflayeringontheformationandgrowthofsolutionpipes
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