| South-Central Section - 39th Annual Meeting (April 1–2, 2005) | |
| Paper No. 5-3 | |
| Presentation Time: 2:30 PM-2:50 PM | ||
STRUCTURAL INFLUENCE ON GROUNDWATER FLOW AS EVIDENCED BY GROUNDWATER DYE TRACING IN THE BARTON SPRINGS SEGMENT OF THE EDWARDS AQUIFER, CENTRAL TEXAS: IMPLICATIONS FOR MODELING CONDUITS | ||
|
HUNT, Brian B.1, SMITH, Brian A.1, BEERY, Joseph1, HAUWERT, Nico M.2, and JOHNS, David A.2, (1) Barton Springs/Edwards Aquifer Conservation District, 1124 Regal Row, Austin, TX 78748, brianh@bseacd.org, (2) Watershed Protection, City of Austin, 206 East 9th Street, Suite 16.100, Austin, TX 78767 Major groundwater flow routes in the Barton Springs segment of the Edwards Aquifer closely follow the structural trends of the Balcones Fault Zone. Locations of these groundwater flow routes and velocities of groundwater flowing along the routes were determined by injecting fluorescent, non-toxic, organic dyes (Fluorescein and Eosine) into two caves within Onion Creek, the largest capacity losing stream in the Barton Springs segment of the Edwards Aquifer. Cripple Crawfish and Antioch caves are located about 17.5 mi and 14.0 mi south of Barton Springs, the primary discharge point from the aquifer, respectively. First arrival of dyes from each of these caves to Barton Springs occurred after about 3.5 and 7.0 days, indicating minimum groundwater velocities under high spring flow and water-level conditions of 5.0 and 2.0 mi/day, respectively. Dye detections at water-supply wells indicate a karst system composed of multiple diverging flow routes from these caves, which appear to re-converge as groundwater flows northeast discharging at Barton Springs. Interpreted flow paths are oriented normal or parallel to potentiometric contours, indicating a highly anisotropic flow system consisting of conduits. Conduit flow within the aquifer appears to be strongly influenced by the bimodal fault and fracture system with trends of N40E (dominant) and N45W (secondary). Groundwater flow was traced in wells along paths that are parallel to the dominant fault trend presented on geologic maps. Groundwater flow was also traced parallel to the secondary structural trend, at a high angle to the dominant mapped fault trend. Results indicate that conduits are an important component of flow, and that the bimodal structural grain has influenced conduit flow in this aquifer. Future numerical groundwater models incorporating conduit flow should consider, among other data, structural grain for modeling the distribution and orientation of conduits. | ||
|
South-Central Section - 39th Annual Meeting (April 1–2, 2005)
General Information for this Meeting | ||
| Session No. 5 Faulting and Related Deformation in the Balcones Fault System and Influence on the Edwards and Trinity Aquifers Trinity University: Stieren Theater 1:40 PM-4:30 PM, Friday, April 1, 2005 Geological Society of America Abstracts with Programs, Vol. 37, No. 3, p. 8 | ||
© Copyright 2005 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||