Name:

Groundwater Resources of the Edwards Aquifer, Texas
Complete the questions below by typing the answers in the boxes and printing the finished form or print the form and write the answers in by hand.  
The Edwards Aquifer is located in a region of rapid population growth centered on the city of San Antonio with a current population of approximately one million people. The aquifer is the major water source for an area that has been affected by long-terms (multiple years) droughts this century. Future growth may make it impossible to continue to divide the aquifer's waters between recreation, agriculture, domestic supply, industry, and wildlife.

Gregg Eckhardt's prize-winning Edwards Aquifer website provides an excellent summary of the geology of the aquifer system and associated water supply issues. Visit the website and answer the questions below.

  1. Water levels in the aquifer are influenced by precipitation. What is the average annual precipitation for the region?

12 inches           20 inches          28 inches          36 inches 

  1. Why is the average precipitation not very useful in planning water use strategies? Describe how precipitation varies with the climate of the region.

  1. What is the rock type of the aquifer?

  1. How does rock type influence porosity and permeability in the aquifer? (Describe how is water stored in the aquifer and how it moves through the aquifer).

  1. How does water enter the aquifer at the recharge zone?

  1. Is the Edwards aquifer an open or closed aquifer?

open                                 closed

  1. Name a rock unit (and include rock type) that lies adjacent to the aquifer that represents an aquiclude.

Water levels in the aquifer will not decline as long as the recharge exceeds the amount of water withdrawn from the aquifer by pumping and by spring flow. Recharge will decline during periods of drought. Spring flow decreased during a multi-year drought in the early 1950's. Examine the graph below and answer the question that follows.
Edwards_graph.gif (11067 bytes) Variations in recharge, spring outflow, and discharge by pumping form the Edwards aquifer from 1938-1992.

Graph modified from Sharp & Banner, 1997, GSA Today, v.7, p.1-9.

  1. Compare the pumping discharge to aquifer recharge values. For approximately how many years would 1992 pumping discharge have exceeded recharge during the time interval represented by the graph?

years

  1. Review information presented at the Edwards Aquifer website and describe any two environmental issues concerning the use of the aquifer that must be resolved in the future.

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