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Gaining vs. losing streams

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Presentation on theme: "Gaining vs. losing streams"— Presentation transcript:

1 Gaining vs. losing streams
Source: U.S.G.S.

2 Effects of pumping on GW - surface water interaction
Source: U.S.G.S.

3 Schematic showing basic elements of an unconfined aquifer system
Source: U.S.G.S.

4 Example of a perched water table and its relationship to the regional unconfined aquifer system

5 Layered aquifer system(s), showing confined aquifer beneath an unconfined aquifer. Note the artesian conditions in the valley.

6 Aquifer in fractured volcanic rocks (Kona, HI)
Source: U.S.G.S. National Groundwater Atlas

7 Regional aquifers in the Mid-Atlantic U.S.
Fractured limestone and metamorphic rock Unconsolidated sediments & sedimentary rock Source: U.S.G.S. National Groundwater Atlas

8 Locations of major sandstone aquifers in the U.S.
Source: U.S.G.S.

9 Example showing porosity (note that for illustration purposes, the sand grains are shown to be unrealistically far apart) Types of porosity

10 Example showing porosity in a thin section of sandstone

11 Hydrostatic Head: An Example...
Which way does the groundwater flow? 10 m 3 m 0 m

12 What is the head at each point?
10 m B Pressure head = 7 m Elevation Head = 3 m Total Head = 10 m 3 m A C 0 m

13 What is the head at each point?
10 m B Pressure head = ?? m Elevation Head = ?? m Total Head = ?? m 3 m A C 0 m

14 What is the head at each point?
10 m B Pressure head = 0 m Elevation Head = 10 m Total Head = 10 m 3 m A C 0 m

15


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