171 D6. The Multidisciplinary Faces of Cave and Karst Science (Posters)

Monday, 23 October 2017
9:00 AM - 6:30 PM
Halls 4EF

SPRINGSHED DELINEATION AT CAVE WITHOUT A NAME, TX, USA:DYE TRACING IN THE LOWER GLEN ROSE LIMESTONE

Paper number: 171-7
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM

Authors

Abstract

Cave Without a Name (CWAN) in Kendall County, TX, USA contains ~5.5 km of active stream conduits formed in the karstic Lower Glen Rose Limestone, which forms part of the Trinity Aquifer System. The primarily rural Kendall County lies just northwest of San Antonio in the Texas Hill Country. The Trinity Aquifer is the primary source of freshwater for this and many other Hill Country counties, although its yields are relatively low compared to the adjacent Edwards Aquifer.

Karst springsheds deliver water to springs via recharge features and conduits or preferential flowpaths and are similar to watersheds, except that their boundaries are not constrained by topography. To delineate the springshed for Cave Without a Name, dye tracing was performed by injecting dyes into recharge features on the land surface. Dye tracing utilizes conservative tracers (dyes) to trace waters from direct recharge sites to a point of discharge (e.g., springs). For this project, multiple traces were performed from sinkholes and/or caves. Regional flow near CWAN is to the Southeast while local flow is towards springs and streams. The Guadalupe River, Spring Creek, and Sabinas Creek are assumed to act as local discharge boundaries, along which a number of known springs occur.

Results of this work support prior work by Veni (1994) that suggested there may be several adjacent springsheds in the area, which is near a large oxbow in the Guadalupe River, just upstream from the confluence with Spring Creek. Groundwater flow velocities as determined by the dye traces ranged from ~0.36 km/day through preferential flowpaths to ~0.02 km/day via diffuse flow through the epikarst. Type of recharge feature, injection method, and hydrologic conditions were found to play significant roles in the behavior of each dye trace. Results of this study can be used as a foundation for future tracing work in the region, and may help with future efforts to manage water quality in the area.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-301782

© Copyright 2017 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.