Pedernales Falls State Park Spring Dye Trace Project: Determining the Source of the Spring at Pedernales Falls State Park

dc.contributor.authorWierman, Douglas A.
dc.contributor.authorWalker, Jenna
dc.contributor.authorMoreno, Jaime
dc.date.accessioned2021-11-12T16:44:11Z
dc.date.available2021-11-12T16:44:11Z
dc.date.issued2017-06
dc.description.abstractThe results of this dye trace study confirm that the source of the spring at the base of the falls at Pedernales Falls State Park (PFSP) is mainly a diversion of river water through a swallet or sink upstream of the park originating in the Marble Falls Formation. Continuous monitoring with a field fluorimeter, charcoal samplers and grab samples of water collected at the spring detected fluorescein dye poured near the area of the swallet. Dye breakthrough at the spring indicated a travel time of approximately 15.5 hours over a 2.4 mile distance.
dc.description.departmentThe Meadows Center for Water and the Environment
dc.formatText
dc.format.extent118 pages
dc.format.medium1 file (.pdf)
dc.identifierReport No. 2017-06
dc.identifier.citationWierman, D. A., Walker, J., & Moreno, J. (2017). Pedernales Falls State Park spring dye trace project: Determining the source of the spring at Pedernales Falls State Park (Report No. 2017-06). Texas State University, San Marcos, Texas.
dc.identifier.urihttps://hdl.handle.net/10877/14826
dc.language.isoenen_US
dc.sourceThe Meadows Center for Water and the Environment. https://www.meadowscenter.txstate.edu/Publications.html
dc.subjectPedernales River
dc.subjectstreams
dc.subjectwater temperature analysis
dc.subjectPedernales Falls State Park
dc.subjectEdwards Aquifer
dc.titlePedernales Falls State Park Spring Dye Trace Project: Determining the Source of the Spring at Pedernales Falls State Park
dc.typeReport

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