Simulation of Flow in the Edwards Aquifer, San Antonio Region, Texas, and Refinement of Storage and Flow Concepts
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LOCAL SPOTLIGHT Edwards Aquifer, San Antonio, Texas, United States—Protecting Groundwater
LOCAL SPOTLIGHT Edwards Aquifer, San Antonio, Texas, United States—Protecting groundwater Photo: © Blake Gordon Photo: © Blake Gordon North America Left. Officials release a benign "tracer dye" into Edwards Aquifer drainage systems to chart flows and track the underground water pathways. Right. Hydrogeologist descends into a sinkhole to check on the Edwards Aquifer. The challenge As one of the largest, most prolific artesian aquifers in the world, the Edwards Aquifer serves as the primary source of drinking water for nearly 2 million central Texans, including every resident of San Antonio—the second largest city in Texas—and much of the surrounding Hill Country. Its waters feed springs, rivers and lakes and sustain diverse plant and animal life, including rare and endangered species. The aquifer supports agricultural, industrial and recreational activities that not only sustain the Texas economy, but also contribute immeasurably to the culture and heritage of the Lone Star State. AUSTIN The aquifer stretches beneath 12 Texas counties, and the land above it includes several important hydrological areas. Two areas in particular— the drainage area and the recharge zone—replenish the aquifer by “catching” rainwater, which then seeps through fissures, cracks and sinkholes into the porous limestone that dominates the region. While this natural filtration system helps refill the aquifer with high-quality water, the growing city of San Antonio is expanding into territories of the very sensitive recharge zone, increasing the risk of contamination. In Edwards Aquifer SAN ANTONIO addition to a rising population, the state’s water supplies have been impacted by multi-year droughts. By 2060, Texas is projected to be home to approximately 50 million people while the annual available water resources are estimated to decrease by nearly 10 percent. -
THURSDAY, NOVEMBER 14, 2013 Grand Hyatt Hotel San Antonio, Texas
THURSDAY, NOVEMBER 14, 2013 Grand Hyatt Hotel San Antonio, Texas THE PRIDE OF TEXAS BUSINESS WELCOME Mark M. Johnson Chairman, Texas Business Hall of Fame Edward E. Whitacre, Jr. Master of Ceremonies RECOGNITION OF TEXAS BUSINESS HALL OF FAME MEMBERS RECOGNITION OF 2013 INDUCTEES INVOCATION Reverend Trey H. Little DINNER RECOGNITION OF 2013 SCHOLARSHIP RECIPIENTS HALL OF FAME INDUCTION CEREMONY CLOSING REMARKS Mark M. Johnson Jordan Cowman Chairman, 2014, Texas Business Hall of Fame 2013 Inductees to the Texas Business Hall of Fame Charlie Amato Joseph M. “Jody” Grant Chairman/Co-Founder Chairman Emeritus and Texas Capital Bancshares, Inc. Gary Dudley Dallas President/Co-Founder SWBC H-E-B San Antonio Represented by Craig Boyan President, COO Tom Dobson San Antonio Chairman Whataburger Rex W. Tillerson San Antonio Chairman and CEO Exxon Mobil Corporation Paul Foster Irving Executive Chairman Western Refining, Inc. El Paso Charlie Amato & Gary Dudley Chairman/Co-Founder & President/Co-Founder SWBC | San Antonio Charlie Amato and Gary Dudley, Co-founders of SWBC, have had a long friendship. Through this friendship, they established SWBC, a company with more than three decades of dedication to not just great business and customer service, but also giving back to their community. Amato and Dudley met in grade school and were reunited in their college years. Both men graduated from Sam Houston State University with Bachelors of Business Administration degrees. After graduation they went their separate ways. Dudley became a coach and worked in the Houston school district for nine months before he was drafted into the armed forces. He spent six months on active duty with the US Marines (and six years as a reservist) before returning to coaching for another year. -
Stewardship of the Edwards Aquifer
STEWARDSHIP OF THE EDWARDS AQUIFER What is the Edwards Aquifer? “The Edwards Aquifer is one of the most valuable resources in the central How does this affect me? Aquifer: an underground area that holds enough water Texas area. In most places, it takes time for stormwater to travel to provide a usable supply. over land and filter through soil to reach the rivers and This aquifer provides water for lakes that supply drinking water to residents. In the municipal, industrial, and agricultural Edwards Aquifer region, recharge features provide a direct link between groundwater and our underground uses as well as sustaining a number of water supply. This means that stormwater pollution rare and endangered species. directly affects the quality of our drinking water. To preserve these beneficial uses, As a result, TCEQ has implemented extra water quality San Antonio ReportSan Texans must protect water quality in requirements to protect the aquifer. Examples include Source: this aquifer from degradation water quality treatments like rain gardens and water resulting from human activities.” quality ponds, as well as erosion and sedimentation While other aquifers in Texas are made up of sand and controls at construction sites. gravel, the Edwards Aquifer is a karst aquifer, composed - Texas Commission on Environmental of porous limestone formations that serve as conduits Quality (TCEQ), RG-348 for water as it travels underground. (Edwards Aquifer Authority) As shown in the graphic to the right, the Edwards Aquifer region encompasses much of South Central Texas. Portions of the City Antonio ReportSan of West Lake Hills lie within the Edwards Aquifer Contributing and Recharge Zones. -
Original TMDL
Upper San Antonio River Watershed Protection Plan SSaa nn AAnnttoonniioo RRiivveerr AAuutthhoorriittyy BBeexxaarr RReeggiioonnaall WWaatteerrsshheedd MMaannaaggeemmeenntt PPaarrttnneerrsshhiipp TTeexxaass CCoommmmiissssiioonn oonn EEnnvviirroonnmmeennttaall QQuuaalliittyy James Miertschin & Associates, Inc. Parsons, Inc. JAMES MIERTSCHIN & ASSOCIATES, INC. ENVIRONMENTAL ENGINEERING P.O. BOX 162305 • AUSTIN, TEXAS 78716-2305 • (512) 327-2708 UPPER SAN ANTONIO RIVER WATERSHED PROTECTION PLAN Prepared For: San Antonio River Authority 100 East Guenther Street San Antonio, Texas 78204 and Bexar Regional Watershed Management Partnership Prepared in Cooperation With: Texas Commission on Environmental Quality The preparation of this report was financed through grants from the Texas Commission on Environmental Quality. Prepared By: James Miertschin & Associates, Inc. Parsons, Inc. December 2006 The Seal appearing on this document was authorized by Dr. James D. Miertschin, P.E. 43900 on 14 Dec 2006. TABLE OF CONTENTS Section Page LIST OF TABLES...............................................................................................................v LIST OF FIGURES ........................................................................................................... vi LIST OF ABREVIATIONS ............................................................................................. vii I. WPP SUMMARY...........................................................................................................1 1.0 INTRODUCTION ...................................................................................................1 -
Comal River's Little-Known Headwaters Nearly Ready for Debut
Local Comal River’s little-known headwaters nearly ready for debut By Brendan Gibbons | September 11, 2017 | Updated: September 11, 2017 10:41pm 0 Photo: John Davenport, STAFF / San Antonio Express-News IMAGE 12 OF 14 Blieders Creek flows Thursday September 7, 2017 next to the Headwaters at the Comal site in New Braunfels, Texas. The site contains the headwaters of the Comal Springs, the original water source for the New ... more NEW BRAUNFELS — Most people think that the Comal River begins at Landa Park, a historic public space in the heart of this city on the edge of the Hill Country. Few know that the river’s true origin lies farther upstream, where spring water flows up from the fractured limestone aquifer below and pours across a creek bed. The spring is inaccessible, hidden by trees and a New Braunfels Utilities property at Lakeview Boulevard and East Klingemann Street. This fall, the public will see the headwaters spring up close as NBU completes the first phase of a restoration of the 16-acre property next to the steep slope of the Balcones Escarpment. NBU is calling this spot the Headwaters at the Comal. If all goes as planned, the property will have walking trails, native plant gardens, an outdoor classroom and a “living building,” among other features, by 2021. “This was all asphalt and a maintenance facility yard,” said Headwaters managing director Nancy Pappas, standing in front of mounds of contoured soil during a tour of the construction site Thursday. “What we have done is removed all that impervious cover and brought in soil to create a more natural look to the property, what it might have been like 1,000 years ago,” she said. -
MEXICO Las Moras Seco Creek K Er LAVACA MEDINA US HWY 77 Springs Uvalde LEGEND Medina River
Cedar Creek Reservoir NAVARRO HENDERSON HILL BOSQUE BROWN ERATH 281 RUNNELS COLEMAN Y ANDERSON S HW COMANCHE U MIDLAND GLASSCOCK STERLING COKE Colorado River 3 7 7 HAMILTON LIMESTONE 2 Y 16 Y W FREESTONE US HW W THE HIDDEN HEART OF TEXAS H H S S U Y 87 U Waco Lake Waco McLENNAN San Angelo San Angelo Lake Concho River MILLS O.H. Ivie Reservoir UPTON Colorado River Horseshoe Park at San Felipe Springs. Popular swimming hole providing relief from hot Texas summers. REAGAN CONCHO U S HW Photo courtesy of Gregg Eckhardt. Y 183 Twin Buttes McCULLOCH CORYELL L IRION Reservoir 190 am US HWY LAMPASAS US HWY 87 pasas R FALLS US HWY 377 Belton U S HW TOM GREEN Lake B Y 67 Brady iver razos R iver LEON Temple ROBERTSON Lampasas Stillhouse BELL SAN SABA Hollow Lake Salado MILAM MADISON San Saba River Nava BURNET US HWY 183 US HWY 190 Salado sota River Lake TX HWY 71 TX HWY 29 MASON Buchanan N. San G Springs abriel Couple enjoying the historic mill at Barton Springs in 1902. R Mason Burnet iver Photo courtesy of Center for American History, University of Texas. SCHLEICHER MENARD Y 29 TX HW WILLIAMSON BRAZOS US HWY 83 377 Llano S. S an PECOS Gabriel R US HWY iver Georgetown US HWY 163 Llano River Longhorn Cavern Y 79 Sonora LLANO Inner Space Caverns US HW Eckert James River Bat Cave US HWY 95 Lake Lyndon Lake Caverns B. Johnson Junction Travis CROCKETT of Sonora BURLESON 281 GILLESPIE BLANCO Y KIMBLE W TRAVIS SUTTON H GRIMES TERRELL S U US HWY 290 US HWY 16 US HWY P Austin edernales R Fredericksburg Barton Springs 21 LEE Somerville Lake AUSTIN Pecos -
Archaeological and Historical Assessment of Brackenridge Park City of San Antonio, Texas
Volume 1979 Article 4 1979 Archaeological and Historical Assessment of Brackenridge Park City of San Antonio, Texas Susanna R. Katz Anne A. Fox Follow this and additional works at: https://scholarworks.sfasu.edu/ita Part of the American Material Culture Commons, Archaeological Anthropology Commons, Environmental Studies Commons, Other American Studies Commons, Other Arts and Humanities Commons, Other History of Art, Architecture, and Archaeology Commons, and the United States History Commons Tell us how this article helped you. Cite this Record Katz, Susanna R. and Fox, Anne A. (1979) "Archaeological and Historical Assessment of Brackenridge Park City of San Antonio, Texas," Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: Vol. 1979, Article 4. https://doi.org/10.21112/ita.1979.1.4 ISSN: 2475-9333 Available at: https://scholarworks.sfasu.edu/ita/vol1979/iss1/4 This Article is brought to you for free and open access by the Center for Regional Heritage Research at SFA ScholarWorks. It has been accepted for inclusion in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State by an authorized editor of SFA ScholarWorks. For more information, please contact [email protected]. Archaeological and Historical Assessment of Brackenridge Park City of San Antonio, Texas Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial 4.0 License This article is available in Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: https://scholarworks.sfasu.edu/ita/vol1979/iss1/4 ARCHAEOLOGICAL AND HISTORICAL ASSESSMENT OF BRACKENRIDGE PARK, CITY OF SAN ANTONIO, TEXAS Susanna R. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on January 11, 2012 Geological Society of America Bulletin Structural framework of the Edwards Aquifer recharge zone in south-central Texas David A. Ferrill, Darrell W. Sims, Deborah J. Waiting, Alan P. Morris, Nathan M. Franklin and Alvin L. Schultz Geological Society of America Bulletin 2004;116, no. 3-4;407-418 doi: 10.1130/B25174.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. -
Groundwater Availability of the Barton Springs Segment of the Edwards Aquifer, Texas: Numerical Simulations Through 2050
GROUNDWATER AVAILABILITY OF THE BARTON SPRINGS SEGMENT OF THE EDWARDS AQUIFER, TEXAS: NUMERICAL SIMULATIONS THROUGH 2050 by Bridget R. Scanlon, Robert E. Mace*, Brian Smith**, Susan Hovorka, Alan R. Dutton, and Robert Reedy prepared for Lower Colorado River Authority under contract number UTA99-0 Bureau of Economic Geology Scott W. Tinker, Director The University of Texas at Austin *Texas Water Development Board, Austin **Barton Springs Edwards Aquifer Conservation District, Austin October 2001 GROUNDWATER AVAILABILITY OF THE BARTON SPRINGS SEGMENT OF THE EDWARDS AQUIFER, TEXAS: NUMERICAL SIMULATIONS THROUGH 2050 by Bridget R. Scanlon, Robert E. Mace*1, Brian Smith**, Susan Hovorka, Alan R. Dutton, and Robert Reedy prepared for Lower Colorado River Authority under contract number UTA99-0 Bureau of Economic Geology Scott W. Tinker, Director The University of Texas at Austin *Texas Water Development Board, Austin **Barton Springs Edwards Aquifer Conservation District, Austin October 2001 1 This study was initiated while Dr. Mace was an employee at the Bureau of Economic Geology and his involvement primarily included initial model development and calibration. CONTENTS ABSTRACT .......................................................................................................................................1 INTRODUCTION..............................................................................................................................1 STUDY AREA...................................................................................................................................3 -
Edwards Aquifer Region 1615 N
EDWARDS AQUIFER REGION 1615 N. St Mary’s Street • San Antonio, Texas 78215 • 210.222.2204 • 1.800.292.1047 • www.edwardsaquifer.org Drainage basins in the drainage area collect surface water runoff and funnel it into streams that cross the recharge zone. In the artesian zone, the water fl ows generally from west to east. Water movement through the Edwards Limestone Drainage County Lines is generally slower south and east of the fresh Area EAA Jurisdictional Boundary water zone. This water remains in contact with Recharge San Antonio City Limits the limestone and gypsum longer, allowing NORTH Zone dissolved mineral concentrations to increase Major Rivers to over 1,000 milligrams/liter. Artesian Minor Rivers WEST EAST Zone Intermittent Streams SOUTH How Does The Aquifer Work? Th is generalized diagram of a north-south cross section of the Edwards Aquifer streams that fl ow downhill to the recharge zone. In the recharge zone, where region highlights the key components of the aquifer and how they inter-relate the Edwards Limestone is exposed at the land surface, the water actually enters About 85% of precipitation falling and function to form a natural underground system for storing water. the aquifer through cracks, crevices, caves, and sinkholes, and then percolates on the area is lost back to the further underground into the artesian zone. Here, a complex network of atmosphere by evaporation or Th e Edwards Aquifer is a karst aquifer, which means it consists of porous, interconnected spaces, varying in size from microscopic pores to open caverns, by transpiration of water vapor honeycombed formations of Edwards Limestone and other associated limestones from vegetation. -
The Edwards Aquifer (Part A)
E-PARCC COLLABORATIVE GOVERNANCE INITIATIVE Program for the Advancement of SYRACUSE UNIVERSITY Maxwell School Research on Conflict and Collaboration THE EDWARDS AQUIFER (PART A) Amidst of one of the worst Texas droughts in recent memory, attorney Robert Gulley wondered why he had left his position at an established law practice to take on the position of program director for the Edwards Aquifer Recovery Implementation Program (EARIP). As the program director, Robert now worked for 26 different organizations and his job was to assist them, using a consensus-based stakeholder process, through one of the most contentious and intractable national disputes involving scarce groundwater resources at the Edwards Aquifer, one of the most valuable water resources in the Central Texas area. This dispute had already spanned decades and, to make this task even more daunting, the competing interests on both sides had made numerous unsuccessful attempts over the years to resolve this conflict. Hot weather, droughts, and the resulting conflicts between stakeholders are frequent occurrences in Texas. Robert, who had returned to his home state specifically for this position, knew that this drought would only intensify the tensions amongst the stakeholders involved. The Edwards Aquifer (“Aquifer”) provides approximately 90 percent of the water for over two million people living and working in the South-Central Texas area. The Aquifer supplies the water that services the city of San Antonio and other municipalities; a multi-million agricultural and ranching industry in the western part of the region that views water as a coveted property right; as well as the recreational activities that provide the backbone of the economies of rapidly-growing, nearby cities of San Marcos and New Braunfels (Figure 1). -
Barton Springs Segment of the Edwards (Balcones Fault Zone) Aquifer, Central Texas
OLD G The Geological Society of America Memoir 215 OPEN ACCESS Barton Springs segment of the Edwards (Balcones Fault Zone) Aquifer, central Texas Brian B. Hunt Brian A. Smith Barton Springs/Edwards Aquifer Conservation District, Austin, Texas 78748, USA Nico M. Hauwert Balcones Canyonland Preserve, City of Austin, Austin Water, Wildland Conservation Division, Austin, Texas 78738, USA ABSTRACT The Barton Springs segment of the Edwards (Balcones Fault Zone) Aquifer is a prolifi c karst aquifer system containing the fourth largest spring in Texas, Barton Springs. The Barton Springs segment of the Edwards Aquifer supplies drinking water for ~60,000 people, provides habitat for federally listed endangered salamanders, and sustains the iconic recreational Barton Springs pool. The aquifer is composed of Lower Cretaceous carbonate strata with porosity and permeability controlled by dep- ositional facies, diagenesis, structure, and karstifi cation creating a triple permeability system (matrix, fractures, and conduits). Groundwater fl ow is rapid within an inte- grated network of conduits discharging at the springs. Upgradient watersheds pro- vide runoff to the recharge zone, and the majority of recharge occurs in the streams crossing the recharge zone. The remainder is direct recharge from precipitation and other minor sources (infl ows from Trinity Group aquifers, the San Antonio segment, the bad-water zone, and anthropogenic sources). The long-term estimated mean water budget is 68 ft3/s (1.93 m3/s). The Barton Springs/Edwards Aquifer Conserva- tion District developed rules to preserve groundwater supplies and maximize spring fl ow rates by preserving at least 6.5 ft3/s (0.18 m3/s) of spring fl ow during extreme drought.