LCRA Griffith League Ranch Application (2018)
The Lower Colorado River Authority (LCRA) applied with the Lost Pines Groundwater Conservation District (District) for groundwater operating and transport permits for eight (8) wells, for a total combined maximum annual production of up to 25,000 acre-feet/year on February 21, 2018. The LCRA acquired groundwater rights in the Simsboro and Carrizo-Wilcox aquifers under the approximately 4,847 acre Griffith League Ranch (GLR) property in Bastrop County on January 9, 2015 by Warranty Deed. LCRA requested the permits include a phased approach to increase authorized pumping over time with Phase 1 total combined maximum annual production up to 8,000 acre-feet/year, Phase 2 15,000 acre-feet/year and Phase 3 25,000 acre-feet/year.
LCRA claims it has existing firm contractual commitments in excess of 400,000 acre-feet/year for a variety of beneficial uses, including municipal, industrial, recreation, irrigation/agricultural and instream uses. With few exceptions LCRA claims that the contractual commitments generally provide that LCRA may meet its obligations from any source available to LCRA.
The map on the right shows the location of the proposed well-field site in Bastrop County, TX. The well-field is approximately northeast of FM1441 and northwest of HWY 21 going northeast out of Bastrop.
Schedule for Public Hearing and Deadline for Registering Objections
The District has indicated the following tentatively scheduling for proceedings associated with the LCRA Griffith League Ranch Application as follows:
June 20, 2018: The District has indicated that LCRA has been requested to provide a public presentation on the application at the District’s regularly scheduled meeting on June 20, 2018 to be held in Giddings, TX.
June 22, 2018: IMPORTANT DATE for any person objecting to the application. In compliance with the District’s rules, June 22, 2018, is the deadline to formally object to the LCRA Griffith League Ranch Application and request a contested case hearing. For more information on requesting a contested case hearing review Rule 15.1.E on page 41 of the District’s Rules.
June 27, 2018: The District has indicated that the required public hearing on the application is tentatively scheduled for June 27, 2018; location to be determined.
Environmental Stewardship will attempt to notify persons who have signed up for our Newsletter about the date, time and other details regarding the above meetings and dates (see “Sign Up For Our Newsletter” below).
The following maps show the other non-exempt well fields in the near the LCRA Griffith Ranch project (left) and the drawdown in the Simsboro aquifer that is predicted to result from the pumping of 25,000 ac-ft/year over a period of 50 years (right).
A recent study predicts that the combined pumping of the Simsboro Aquifer will impact other shallower aquifers in the Carrizo-Wilcox Group. THE STUDY DID NOT INCLUDE THIS LCRA GRIFFITH LEAGUE RANCH PROJECT.
The combined pumping in the Simsboro Aquifer is predicted to cause 900 to 1200 feet of drawdown in the Simsboro Aquifer in Burleson and Lee counties by the year 2060 according to groundwater modeling conducted by professional hydrologist George Rice. The groundwater pumping within Lost Pines and Post Oak Savannah Groundwater Conservation Districts (GCD) are predicted to impact not only the Simsboro Aquifer, but also the Carrizo, Calvert Bluff and Hooper aquifers extending to points as far away as Gonzoles, Lavaca, Colorado, Austin, Grimes and Walker counties. These aquifers are hydraulically connected throughout the Carrizo-Wilcox Aquifer Group.
Leakage from the Carrizo, Calvert Bluff, and Hooper aquifers
According to the Rice report, the effects of the pumping would not be limited to the Simsboro Aquifer. The pumping would induce leakage from the Carrizo, Calvert Bluff, and Hooper aquifers. This leakage would reduce hydraulic heads in the aquifers. Where the aquifers are confined, the reduction in heads would reduce water levels in wells that draw water from the aquifers. Where the aquifers are unconfined (the shallow outcrop areas where many domestic wells are located), the reduction in heads would dewater portions of the aquifers. The position of these aquifers relative to the Simsboro is shown in figure 1.
Leakage is a common and well-known phenomenon that is discussed in standard hydrology texts. In figure 1, leakage (cross-formational flow) between geologic units is indicated by double-headed arrows. In a 2009 pump-test conducted in Lee County, it was estimated that 22% of the water pumped from the Simsboro was derived from leakage from adjacent aquifers.
Depending on where a Landowner’s property is located in the outcrop, the aquifers beneath the property will be the ones listed below the location. For example, if the property is in the Carrizo outcrop, the aquifers below the property are the Wilcox/Calvert Bluff, Wilcox/Simsboro, and the Wilcox/Hooper; in that order. A landowner owns the groundwater beneath his/her property in ALL of those aquifers.
The maps below show the approximate location of the LCRA Griffith League Ranch Project over the Carrizo, Calvert Bluff, Simsboro, and Hooper Aquifers.
The LCRA Griffith League Ranch Project is likely located in the Carrizo and/or Calvert Bluff aquifer outcrops. Landowners should find the general location of their property and wells on the maps below to be able to estimate the feet of predicted drawdown under their property within the 50 year planning period.
Click on each map to see a larger view of the map.