| 2007 GSA Denver Annual Meeting (28–31 October 2007) | |
| Paper No. 11-2 | |
| Presentation Time: 8:15 AM-8:30 AM | ||
AQUIFER DELINEATION FOR GROUNDWATER MANAGEMENT IN A DEVELOPING ARID KARSTIC BASIN: CUATROCIÉNEGAS, COAHUILA, MEXICO | ||
|
WOLAVER, Brad D., Geological Sciences, The University of Texas at Austin, Jackson School of Geosciences, Austin, TX 78712-0254, brad_wolaver@yahoo.com and SHARP, John M. Jr, Geosciences, The University of Texas at Austin, Austin, TX 78705 This research uses an integrative approach to delineate recharge pathways to springs in the arid karstic Cuatrociénegas Basin, Coahuila, Mexico, using sparse hydrogeologic data (spring water geochemistry, isotopes, temperature, and discharge), catchments delineated in GIS, surface geophysics, and geologic maps. Springs occur in lines parallel to the Sierra San Marcos, a 2,300-m high Cretaceous carbonate anticline that divides the 1,200 km2 valley into west and east sub-basins. Groundwater-dependent ecosystems in this UNESCO Reserve host over 70 endemic species threatened by groundwater pumping in adjacent valleys. Few hydrogeologic data exist and the location and timing of recharge are poorly constrained; this complicates recharge area delineation and groundwater management. Analysis of tritium and stable isotope (2H and 18O) of the springs suggest older regional groundwater flow predominate with younger local recharge also occurring between 1,500 and 2,300 m – the elevation of mountains surrounding the Cuatrociénegas Basin and throughout the Sierra Madre Oriental of northeast Mexico. The hydrogeologic model is distinct for east and west sub-basin springs. The west sub-basin contains fracture-controlled springs with relatively high and constant discharge, elevated temperatures, and high conductivity. The east sub-basin is comprised of dozens of stratigraphically-controlled small springs adjacent to alluvial fans with lower temperature, lower conductivity, and relatively low discharge affected by precipitation. Noble gas analysis and tritium/helium (3H/3Hetrit) age dating of basin-wide springs suggest mountain recharge older than 50 years predominates. The springs discharge from both regional flow systems and local mountain recharge so that management should also be regional extending beyond the Cuatrociénegas Basin. The approach can be applied to similar developing aquifer systems globally with sparse hydrogeologic data. | ||
|
2007 GSA Denver Annual Meeting (28–31 October 2007)
General Information for this Meeting | ||
| Session No. 11 Springs and Spring Deposits Colorado Convention Center: 708/710/712 8:00 AM-12:00 PM, Sunday, 28 October 2007 Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 37 | ||
© Copyright 2007 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. | ||