Abstract
The Cretaceous-age Middle Trinity Aquifer in central Texas exhibits significant karst features where it is exposed at the surface.Where these units are overlain by the karstic Upper Trinity and Edwards Aquifers, the degree of karstification is not known, but groundwater in certain units of the Middle Trinity Aquifer is chemically similar to shallow groundwater in this area. Geochemical, potentiometric, and hydraulic conductivity data suggest that this deep groundwater is following pathways from the recharge areas that allow for rapid flow compared to other deep units that contain waters of significantly different chemistry. A 340-m deep multiport monitor well was installed in the Edwards (shallowest), and Upper and Middle Trinity Aquifers to better understand the vertical and horizontal relationships of these aquifers. The well was completed with 14 monitor zones allowing for groundwater sampling, hydraulic conductivity testing, and pressure measurements (potentiometric levels) in each zone. Data from this well suggest that karstification processes are active at depths of 300 m below land surface in a confined aquifer at least 25 km from the closest recharge areas.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Ashworth, JB (1983) Ground-Water Availability of the Lower Cretaceous Formations in the Hill Country of South-Central Texas: Texas Department of Water Resources, Report 273, 172Â p
Collins, EW (1995) Structural framework of the Edwards Aquifer, Balcones Fault Zone, central Texas: Gulf Coast Association of Geological Societies Transactions, vol. 45, pp. 135–142
Collins, EW, and Hovorka, SD (1997) Structure map of the San Antonio segment of the Edwards Aquifer and Balcones Fault Zone, south-central Texas: structural framework of a major limestone aquifer: Kinney, Uvalde, Medina, Bexar, Comal and Hays Counties: The University of Texas at Austin, Bureau of Economic Geology, Miscellaneous Map No. 38, scale 1:250,000, text 14 p
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2010 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Smith, B., Hunt, B. (2010). Flow Potential Between Stacked Karst Aquifers in Central Texas, USA. In: Andreo, B., Carrasco, F., Durán, J., LaMoreaux, J. (eds) Advances in Research in Karst Media. Environmental Earth Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-12486-0_7
Download citation
DOI: https://doi.org/10.1007/978-3-642-12486-0_7
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-12485-3
Online ISBN: 978-3-642-12486-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)