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Groundwater PowerPoint PPT Presentation

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Groundwater. Importance of Groundwater. Supplies 40% of U.S. public drinking water. Almost all rural residents Agriculture can be dependent on groundwater for irrigation. Shapes the land surface (e.g. sinkholes, mudslides). Fig. 17.3. Occurrence of Groundwater.

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Importance of groundwater

Importance of Groundwater

  • Supplies 40% of U.S. public drinking water.

    • Almost all rural residents

  • Agriculture can be dependent on groundwater for irrigation.

  • Shapes the land surface (e.g. sinkholes, mudslides).

Fig. 17.3

Occurrence of groundwater

Occurrence of Groundwater

  • Found everywhere below the surface, in all rock/sediment types.

  • Stored in and flows through pores spaces.

Fig. 17.5

Fig. 17.5

Occurrence of groundwater1

Occurrence of Groundwater

  • The watertable is the boundary between the unsaturated and saturated zones.

Unsat. – pores filled with air and water

Sat. – pores filled with only water

Fig. 17.6

Occurrence of groundwater2

Occurrence of Groundwater

  • Most surface water bodies (i.e. streams, lakes) occur where water table insects the land surface.

Quarries/mines must be dewatered while operating.

Fig. 17.4

Movement of groundwater

Movement of Groundwater

  • Precipitation infiltrates, flows through unsat. zone to water table.

  • Groundwater flows from higher to lower elevations (velocity – cm to m per day).

Fig. 17.17

The water table and groundwater flow

The Water Table and Groundwater Flow

Water table fluctuations

Water Table Fluctuations

  • The water table is continually rising and falling.

    • rises when precipitation infiltrates

    • falls as water discharges to streams

Fig. 17.13

Water table fluctuations1

The water table also drops when water is pumped from wells.

Water Table Fluctuations

  • Shallow wells go dry during dry periods.

  • water table drops below bottom of the well.

Effects of pumping groundwater

Effects of Pumping Groundwater

Effects of pumping groundwater1

Effects of Pumping Groundwater

  • Groundwater can be pumped out faster than it recharges.

    • water table drops, aquifer yields less water

Fig. 17.13

Effects of pumping groundwater2

Effects of Pumping Groundwater

Fig. 17.14

  • High Plains Aquifer:

    • Low recharge rate

    • High pumping rate (agriculture)

    • Max. water table drop is >50 m (160 ft.)

    • Half of aquifer has been drained

Effects of pumping groundwater3

Effects of Pumping Groundwater

Fig. 17.33

  • Land subsidence:

  • Water in pores supports grains, resists compaction.

  • Dewatering pores allows compaction.

  • Compaction lowers land surface elevation (subsidence).

Effects of pumping groundwater4

Effects of Pumping Groundwater

  • Land subsidence fissures in Arizona caused by groundwater pumping.

Fig. 17.15

Effects of pumping groundwater5

Effects of Pumping Groundwater

Fig. 17.33

  • Salt water intrusion:

  • Near coasts, groundwater at depth is salty.

  • Pumping fresh water may eventually draw salt water into a well.

Groundwater and landscapes

Groundwater and Landscapes

  • Limestone is easily dissolved by groundwater.

  • Sinkholes – where surface rocks collapse into the void left after limestone dissolves.

Fig. 17.36

Groundwater and landscapes1

Groundwater and Landscapes

  • Groundwater flows along joints, dissolves limestone.

  • Eventually, caves form and sinkholes form when cave roof collapses.

Fig. 17.36

Groundwater and landscapes2

Groundwater and Landscapes

  • Sinkhole damage in Florida.

Groundwater and landscapes3

Groundwater and Landscapes

  • Areas in the U.S. where rocks are easily dissolved.

Fig. 17.36

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