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Aquifers/Edwards Aquifer

Date post: 08-Feb-2016
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Aquifers/Edwards Aquifer. What is an Aquifer ? A body of rock, sediment, or soil that contains drinkable water and can transmit this water to wells or springs in economically usable quantities. 3 Major Types of Aquifers. 1. Unconfined (most common) 2. Confined - PowerPoint PPT Presentation
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Page 1: Aquifers/Edwards Aquifer

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Aquifers/Edwards Aquifer

Page 2: Aquifers/Edwards Aquifer

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What is an Aquifer?

A body of rock, sediment, or soil that contains drinkable water and can transmit this water to wells or springs in economically usable quantities

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3 Major Types of Aquifers

1. Unconfined (most common)

2. Confined

3. Karst: a special type that occurs in limestone rocks when a system of caves is connected and water is flowing through it. –Edwards Aquifer

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Unconfined Aquifer

Water seeps through porous materials near the surface, but is trapped by impermeable rock below.

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Confined Aquifer

Impermeable rock above and below. Rock strata must bend and outcrop at surface for rain to recharge porous material in between.

Water will pressurize if higher than well heads – artesian system

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Karst Aquifer

Develops in thick limestone formations, usually in humid climates. Karst has both surface and subsurface features.

http://www.watersheds.org/earth/Sinkholes.html

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Water naturally goes underground through sinkholes to caves (solution caverns).

Rainwater is slightly acidic and dissolves limestone rock to calcium carbonate & carries it away (dissolution).

Causes stalactite, stalagmite, & pillar formations in caverns

Karst Aquifer

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Recharge Zone

Drainage Area

Artesian Zone

Source: Edwards Aquifer Authority, 2002

Edwards AquiferAquifer Region and Authority Boundaries

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Edwards Aquifer in Bexar County

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Geologic HistoryAbout 17 million years ago, the aquifer rockswere uplifted and faulted, forming the BalconesEscarpment. They became subject to erosion anddissolution.

http://www.watersheds.org/earth/karstmovie.htm

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Edwards Aquifer Cross Section

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Recharge Zone• Water enters the aquifer

through faults, fractures, sinkholes, or percolation through the soil. This process is called recharge.

• The recharge zone is the area where water enters the aquifer.

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Caves Associated With the Edwards Aquifer

Devil’s Sinkhole State Natural Area

Rocksprings, TX

Natural Bridge CavernsNatural Bridge Caverns,

TX

Kickapoo Caverns State ParkBrackettville, TX

Inner Space CavernAustin, TX

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Flowpaths of the Edwards Aquifer

Why does the water flow in the direction shown in the figure? Elevation

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The aquifer contains severalflow systems – One occursnear Del Rio

Flowpaths of the Edwards Aquifer

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Flowpaths of the Edwards Aquifer

The largest flow system runsfrom near Brackettville to nearKyle…

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… and supplies the major springs at

San Marcos, New Braunfels, andSan Antonio.

Flowpaths of the Edwards Aquifer

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Smaller flow systems include theBarton springs flow system…

Flowpaths of the Edwards Aquifer

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Flowpaths of the Edwards Aquifer

…and areas north of theColorado River .

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How does the water come out & who uses it?

Aquarina SpringsSan Marcos, TX

1 Million gallons of water released from the ground per day

Wells & Springs

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Barton (main) Spring

Austin, TX

Austin

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San Marcos Springs

San Marcos, TX

San Marcos

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Del Rio

San Felipe

SpringsDel Rio,

TX

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Water Supply Problems

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Water Supply Problems

http://www.watersheds.org/earth/karstmovie.htm

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EndangeredComal Springs Dryopid Beetle Comal Springs Riffle BeetleFountain Darter Peck’s Cave AmphipodSan Marcos Gambusia Texas Blind SalamanderTexas wild-rice

ThreatenedSan Marcos Salamander

Eight species in the Edwards Aquifer, Comal Springs, and San Marcos Springs ecosystems are currently listed by the U.S. Department of Interior, Fish and Wildlife Service, as either threatened or endangered species.

Environmental Impact


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