A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface
The Edwards aquifer in south-central Texas, U.S., composed of faulted carbonate bedrock, contains freshwater and saline water. In aquifers that are used as a source of drinking water and that contain fresh and saline waters, saline-water intrusion can result in degradation of water quality. Yet, in...
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ndltd-LSU-oai-etd.lsu.edu-etd-05312012-2125452013-01-07T22:53:59Z A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface Tipple, Scott Ryan Geology & Geophysics The Edwards aquifer in south-central Texas, U.S., composed of faulted carbonate bedrock, contains freshwater and saline water. In aquifers that are used as a source of drinking water and that contain fresh and saline waters, saline-water intrusion can result in degradation of water quality. Yet, in the Edwards aquifer, limited saline-water intrusion has occurred. The questions addressed are Why is the saline-water intrusion less than expected, and Is there a trigger that will result in saline-water intrusion into the freshwater reservoir? Three hypotheses were tested. One: an extremely saline water density might prevent mixing across the interface. Two: faults could be acting as a barrier between the freshwater and saline-water zones, preventing movement of the saline water into the freshwater zone. Three: the permeability of the bedrock in the saline water zone might be extremely low, limiting movement of the saline water. A transect of observation wells was chosen in New Braunfels, TX for study. 2-D, variable-density numerical models of groundwater flow were used to determine which factor controlled the lack of saline-water intrusion. Numerical models were produced for each hypothesis using Basin2. It is clear from each model that fault permeability and fault compartmentalization is the primary mechanism inhibiting flow across the freshwater/saline-water interface. When horizontal fault permeability reached 0.01 D, flow was significantly reduced across the interface. When these values reached 0.001 D, flow across the interface ceased. To a lesser extent, saline-water zone permeability controlled the movement of flow across the interface, if permeability values were reduced by three orders of magnitude. However, extremely high saline water densities did not inhibit flow. A trigger that would increase fault permeability would be continued dissolution of the carbonate rocks, but it most likely would take tens of thousands of years for dissolution to significantly increase the permeability of the fault surfaces. In addition, dedolomitization of the saline water zone would be another trigger that would induce flow across the interface, but since little diagenesis in the saline water zone has been observed, dedolomitization is not a pressing issue. Wicks, Carol Hanor, Jeffrey Nunn, Jeffrey LSU 2012-06-06 text application/pdf http://etd.lsu.edu/docs/available/etd-05312012-212545/ http://etd.lsu.edu/docs/available/etd-05312012-212545/ en unrestricted I hereby certify that, if appropriate, I have obtained and attached herein a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to LSU or its agents the non-exclusive license to archive and make accessible, under the conditions specified below and in appropriate University policies, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report. |
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Geology & Geophysics Tipple, Scott Ryan A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
description |
The Edwards aquifer in south-central Texas, U.S., composed of faulted carbonate bedrock, contains freshwater and saline water. In aquifers that are used as a source of drinking water and that contain fresh and saline waters, saline-water intrusion can result in degradation of water quality. Yet, in the Edwards aquifer, limited saline-water intrusion has occurred. The questions addressed are Why is the saline-water intrusion less than expected, and Is there a trigger that will result in saline-water intrusion into the freshwater reservoir? Three hypotheses were tested. One: an extremely saline water density might prevent mixing across the interface. Two: faults could be acting as a barrier between the freshwater and saline-water zones, preventing movement of the saline water into the freshwater zone. Three: the permeability of the bedrock in the saline water zone might be extremely low, limiting movement of the saline water. A transect of observation wells was chosen in New Braunfels, TX for study.
2-D, variable-density numerical models of groundwater flow were used to determine which factor controlled the lack of saline-water intrusion. Numerical models were produced for each hypothesis using Basin2. It is clear from each model that fault permeability and fault compartmentalization is the primary mechanism inhibiting flow across the freshwater/saline-water interface. When horizontal fault permeability reached 0.01 D, flow was significantly reduced across the interface. When these values reached 0.001 D, flow across the interface ceased. To a lesser extent, saline-water zone permeability controlled the movement of flow across the interface, if permeability values were reduced by three orders of magnitude. However, extremely high saline water densities did not inhibit flow.
A trigger that would increase fault permeability would be continued dissolution of the carbonate rocks, but it most likely would take tens of thousands of years for dissolution to significantly increase the permeability of the fault surfaces. In addition, dedolomitization of the saline water zone would be another trigger that would induce flow across the interface, but since little diagenesis in the saline water zone has been observed, dedolomitization is not a pressing issue.
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author2 |
Wicks, Carol |
author_facet |
Wicks, Carol Tipple, Scott Ryan |
author |
Tipple, Scott Ryan |
author_sort |
Tipple, Scott Ryan |
title |
A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
title_short |
A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
title_full |
A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
title_fullStr |
A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
title_full_unstemmed |
A 2-D, Variable-Density Numerical Model of Subsurface Fluid Flow through the Edwards Aquifer, New Braunfels, TX: Mechanisms Inhibiting Flow across the Freshwater/Saline-Water Interface |
title_sort |
2-d, variable-density numerical model of subsurface fluid flow through the edwards aquifer, new braunfels, tx: mechanisms inhibiting flow across the freshwater/saline-water interface |
publisher |
LSU |
publishDate |
2012 |
url |
http://etd.lsu.edu/docs/available/etd-05312012-212545/ |
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