© 2012 John Wiley & Sons, Inc. All rights reserved. Chapter 11: Water On and Under the Ground...
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Transcript of © 2012 John Wiley & Sons, Inc. All rights reserved. Chapter 11: Water On and Under the Ground...
© 2012 John Wiley & Sons, Inc. All rights reserved.
Chapter 11: Water On and Under the Ground
Victoria Falls, Zambezi River, southern Africa
Learning ObjectivesThe hydrologic cycle• Describe the hydrologic cycle and its main
pathways and reservoirs.
How water affects land• Contrast the properties and actions of
streams, channels, and lakes.
Water as a hazard and a resource• Explain how floods occur and why prevention
efforts sometimes make flooding worse.
Fresh water underground• Describe the water table and the movement,
storage, and depletion of groundwater.© 2012 John Wiley & Sons, Inc. All rights reserved.
The Hydrologic Cycle
Hydrology• The scientific study of water.
Evaporation• Water changes from a liquid into water.
Transpiration• Water taken up by plants passes into the
atmosphere.
Condensation• Water changes from a vapor into a liquid or
a solid.
© 2012 John Wiley & Sons, Inc. All rights reserved.
© 2012 John Wiley & Sons, Inc. All rights reserved.
The Hydrologic Cycle
Figure 11.1a The hydrologic cycle
The Hydrologic Cycle
Figure 11.2 Reservoirs in the hydrologic cycle
© 2012 John Wiley & Sons, Inc. All rights reserved.
The Hydrologic Cycle
Figure 11.2a Salt water
Figure 11.2b Frozen
Figure 11.2c Underground
Figure 11.2d Surface and atmosphere
© 2012 John Wiley & Sons, Inc. All rights reserved.
The Hydrologic Cycle
Figure 11.3 Living on the water’s edge, Mississippi River, St. Louis, MO
© 2012 John Wiley & Sons, Inc. All rights reserved.
How Water Affects LandStreams and Channels
• Stream• A body of water
that flows downslope along a clearly defined natural passageway
Figure 11.4a Straight channel
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Figure 11.4c Braided channel
© 2012 John Wiley & Sons, Inc. All rights reserved.
•Channel• The clearly
defined passageway through which a stream flows:• Straight• Meandering• Braided
How Water Affects LandStreams and Channels
Figure 11.4b Meandering channel
•Gradient• The steepness of a
stream channel•Discharge
• The mount of water passing by a point on a channel’s bank during a unit of time
•Load• The suspended and
dissolved sediment carried by a stream
Figure 11.5 A river changes shape
© 2012 John Wiley & Sons, Inc. All rights reserved.
How Water Affects LandStreams and Channels
• Floodplain• The relatively
flat valley floor adjacent to a stream channel,
• Inundated when the stream overflows its banks
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Figure 11.6a Floodplain
How Water Affects LandStream Deposits
• Alluvium• Stream sediment• Unconsolidated
sediment • Recently
deposited (geologically speaking)
Figure 11.6b Alluvial fan, Badwater fan, Badwater, Death Valley
© 2012 John Wiley & Sons, Inc. All rights reserved.
How Water Affects LandStream Deposits
• Delta• Sedimentary
deposit, commonly triangular, that forms where a stream enters a standing body of water
Figure 11.6c Nile River delta
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How Water Affects LandStream Deposits
Figure 11.7 Disappearing coastline, Mississippi River delta
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How Water Affects LandStream Deposits
How Water Affects LandLarge-Scale Topography of Stream Systems
Figure 11.8 Mississippi River drainage basin
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What a Geologist Sees—Drainage Basins
Drainage basin of Wadi Al Masilah, south Yemen
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• Drainage basin• The total area from
which water flows into a stream
• Divide• A topographic high
that separates adjacent drainage basins
Figure 11.9 Continental drainage in the Americas
© 2012 John Wiley & Sons, Inc. All rights reserved.
How Water Affects LandLarge-Scale Topography of Stream Systems
How Water Affects LandLakes
Lakes are standing bodies of water that have open surfaces, in direct contact with the atmosphere.
Figure 11.10 A dying river from eutrophication © 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a Resource
Floods• An event in which
a body of water overflows its banks
Flood prediction and prevention
• Flood-frequency curve
• Recurrence interval
• Channelization
Figure 11.11a Mississippi River flood
© 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a Resource
Figure 11.11b Mississippi River flood, May 2011
© 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a Resource
Hydrograph•Graph plotting discharge vs. time to record the flooding of a stream
Figure 11.12 A hydrograph or stream discharge
© 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a Resource
Figure 11.13 Coastal flooding
© 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a Resource
Figure 11.14 Predicting floods© 2012 John Wiley & Sons, Inc. All rights reserved.
Flood-frequency curve•Floods of different magnitudes are plotted on a graph for a given river.
Water as a Hazard and a ResourceSurface Water Resources
• Reliable water supply is critical to human survival and health, agriculture, and other economic activities.
• Nearly 250 million people are designated as water-scarce.
© 2012 John Wiley & Sons, Inc. All rights reserved.
Water as a Hazard and a ResourceSurface Water Resources
Figure 11.15 Principal watersheds of the world
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Case Study: Mono Lake
a. Calcium carbonate spires form under water
b. Water is now fed back into Mono lake
c. Probably just in time to save the California gull
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water Underground
•Groundwater• Subsurface
water contained in pore spaces in regolith and bedrock
•Water table• The top surface
of the saturated zone
Figure 11.16 Water under the ground
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water Underground
How groundwater moves•Porosity
• The percentage of the total volume of a body of rock or regolith that consists of open spaces (pores)
•Permeability• Measure of how easily a
solid allows fluids to pass through it
Figure 11.17 Porosity in rocks and sediment
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water UndergroundHow Groundwater Moves
•Percolation• Groundwater
seeps downward• Flows under the
influence of gravity
•Recharge• Replenishment of
groundwaterFigure 11.18 How groundwater flows
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•Discharge• Subsurface water
leaves the saturated zone
• Becomes surface water
•Spring• Occurs where the
water table intersects the land surface
Figure 11.21a Spring in the Grand Canyon
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water UndergroundHow Groundwater Moves
• Aquifer• A body of rock or
regolith that is water saturated, porous, and permeable
• Aquiclude• A layer of
impermeable rock• Artesian well Figure 11.19 Aquifers, confined and unconfined
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water UndergroundWhere Groundwater Is Stored
Figure 11.20a Artesian water Figure 11.20b Frozen artesian well, New York
© 2012 John Wiley & Sons, Inc. All rights reserved.
Fresh Water UndergroundWhere Groundwater Is Stored
Fresh Water Underground
Figure 11.22 Wells: year-round and seasonal
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Fresh Water Underground
Figure 11.23 Subsidence
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Fresh Water Underground
Figure 11.24 The forgotten oil spill
© 2012 John Wiley & Sons, Inc. All rights reserved.
Freshwater UndergroundWhen Groundwater Dissolves Rock
•Karst topography•Sinkholes•Cave• Underground open
space• A cavern is a system
of connected caves
Figure 11.25 a & b Karst
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Amazing Places: Lechuguilla Cave
a. A bush of aragonite
c. “Pool fingers”
b. Soda straws
d. Gypsum crystals
© 2012 John Wiley & Sons, Inc. All rights reserved.
Critical Thinking
• List the many ways we depend on the availability of fresh water in our daily lives.
• Where does your community obtain its water supply (i.e., groundwater, surface source)? Is the quantity or the quality of the water threatened?
• What would happen to the sea level and the shoreline if great ice sheets built up on the land?
© 2012 John Wiley & Sons, Inc. All rights reserved.