GSA Annual Meeting in Seattle, Washington, USA - 2017

Paper No. 171-7
Presentation Time: 9:00 AM-6:30 PM

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


HILER, Mark D., Texas State University, 601 University Drive, San Marcos, TX 78666, SCHWARTZ, Benjamin F., Edwards Aquifer Research and Data Center, and Department of Biology, Texas State University, Freeman Aquatic Station, 601 University Drive, San Marcos, TX 78666 and SCHINDEL, Geary M., Edwards Aquifer Authority, Aquifer Management, 900 E. Quincy, San Antonio, TX 78215, markhiler@txstate.edu

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.