Download - Water Systems
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Water Systems
The Water Cycle, Streams, and Ground Water
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Earth’s Water Supply
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Water Cycle• movement of water between the atmosphere, the land,
and the oceans.
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Evaporation
• Water changing from liquid phase to a gaseous phase(water vapor) without boiling.
• Surface 2/3 Water• 500,000 km3 /year• Evapotranspiration – evaporation from plant
leaves.
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Condensation• change of state from a gas to a liquid• When water vapor rises in the atmosphere, it
expands and cools.• As the vapor becomes cooler; some of it
condenses back to liquid• High – Clouds• Low – Fog• Surface - Dew
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Precipitation• Any form of water that falls to Earth’s surface (rain,
snow, sleet, and hail)
• Most precipitation falls on Earth’s oceans.
• The rest falls on land and becomes runoff or infiltrates the soil to become groundwater.
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Runoff
• Rain that falls to the ground and is not absorbed
• Moves along the surface of the land until it flows into a stream system
• Causes erosion.
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Factors Affecting Runoff
Rate of rain Runoff
Slope Runoff
Buildings Runoff
Plants Runoff
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River Systems• watershed (AKA basin) the area of land that is
drained by a river system
• The ridges or elevated regions that separate watersheds are called divides.
• tributaries streams that flows into a lake or into a larger stream
• A river system is made up of a main stream and tributaries.
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Mississippi River Basin
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MooseheadLake
WatershedContains:• 31 lakes• 549 m2 of land •400 miles of rivers and streams•empties out into the Atlantic Ocean
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River Systems• Channel - Depression that a stream follows as it
flows downhill
• Banks - The edges of a stream channel that are above water level
• Bed - The part of the stream channel that is below the water level
• A stream channel gradually becomes wider and deeper as it erodes its banks and bed.
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River Systemsstream load - Sediment carried by a stream
• Stream load takes three forms– suspended load
– bed load
– dissolved load
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Stream Load
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River SystemsStream gradient the change in elevation over a given
distance• Near the headwaters, or the beginning of a stream,
the gradient generally is steep.
• As the stream nears its mouth, its gradient often becomes flatter.
• The characteristics of streams with different gradients are very different
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Gradient
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River Systems• River systems change continuously because of
erosion.• Depending on the slope of the land, streams
have three stages of development. Young, Mature, and Old
• These differing streams support different types of organisms
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Young Streams
• Flow swiftly through a steep valley.• Lots of whitewater and waterfalls because
they have not yet eroded all the material in their way.
• Young streams erode most on the bottom and less on the sides.
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Qualities
• Fast Moving• High oxygen• Cold• Little Nutrients
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Stream Merging
• Many young streams join together to form larger streams.
• Depending on the slope of the land and the amount of water they will form either mature or old streams
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Mature and Old Streams
• Mature and Old Streams flow through floodplains.
• floodplain an area along a river that forms from sediments deposited when the river overflows its banks
• Occurs when water levels increase depending on the amount of rainfall and snowmelt in the watershed.
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Floodplains
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Mature Streams
• Curving streams that flow down a gradual slope
• Erode more on their sides than on the bottom.
• This leads to the creation of meanders (curves in a stream)
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Qualities
• Lots of sediment/nutrients – Erosion from young streams
• Slow moving– Algae can grow
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Evolution of Mature Streams
meander• When a river rounds a bend, the velocity of the
water on the outside of the curve increases. – Increase erosion
• On the inside of the curve, the velocity of the water decreases. – Increased deposition
• Causes curves to widen
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Stream Flow
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HorseshoeBend
of the Colorado River near Page, AZ
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Oxbow Lakes
• The curve enlarges while further erosion takes place on the opposite bank, where the water is moving more quickly.
• Meanders can become so curved that they almost form a loop, separated by only a narrow neck of land
• This can eventually become separated into an oxbow lake
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Old Streams
• Old streams flow very slowly through a broad flat floodplain.
• Usually they have lost their meanders and flow more straightly.
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Deltas and Alluvial Fans• Fan-shaped masses of sediment deposited as a
stream slows
• Deltas occur where streams meet oceans
• Alluvial fans result where streams loose energy as the slope decreases rapidly.
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Groundwater
• Water that absorbs into the ground and is located in the spaces between sediments (pores)
• These pores are connected and allow water to flow through them.
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Permeability
• Ability of a material(rock/sediment) to allow water to flow through it.
• Permeable rock/sediment layers allow water to pass through easily
• Impermeable rock/sediment layers resist the flow of water.
• Depends on size and shape of sediment
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Zone of Saturation
• Ground water fills the pores in the permeable rock/sediment layer creating an aquifer.
• The area of the soil where all of the pores have completely filled with water is referred to as the zone of saturation.
• The upper limit of this zone is called the water table.
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Wells
• Holes that are dug below the water table.
• Water has been filtered by sediment.
• If water table drops (drought) it can dry up the well.
• Too many wells in one area can also lower the water table
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Artesian Wells
• Special kind of well where water is pushed up to the surface naturally.
• Require a special kind of geography where an aquifer is sandwiched between impermeable layers and the layers change in elevation.
• Gravity creates pressure that forces water up artesian wells.
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Springs• Springs can exist where the groundwater
reaches the surface
• Some times cracks allow natural artesian wells to form.
• Freshwater springs exist along coasts where fresh ground water enters the ocean.
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Hot Springs and Geysers
• Occur where groundwater is stored near hot rocks
• Hot springs - near boiling water leaks up to the surface.
• Geysers - boiling water and steam is periodically released causing a stream of hot water to shoot out of the ground.
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Caves and Sinkholes
• Form as carbonic acid dissolves limestone.
• Caves are structurally stable and do no collapse.
• If soil above a cave is weak and it collapses into a sinkhole.
• People pumping water out can turn caves into sink holes
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Stalactites and Stalagmites
• Little CO2 in caves, carbonic acid breaks down, can’t hold dissolved limestone.
• Limestone accumulates as water drips
• Stalactite - ceiling of the cave • Stalagmite - ground of the cave
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QuickTime™ and a decompressor
are needed to see this picture.
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Adaptations
• Animals must have special adaptations to deal with living in a cave
• Dark• No plants• Wet• Dangerous Chemicals