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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Online Access: | http://journal.frontiersin.org/Journal/10.3389/fphy.2015.00092/full |
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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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1725501390504067072 |