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Rivers and Streams Courtney Monroe February 30, 2012

Rivers and Streams

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Rivers and Streams. Courtney Monroe February 30, 2012. Water Cycle ~ the movement of H 2 O through the hydrosphere, and other spheres. Water Cycle ~ the movement of H 2 O through the hydrosphere, and other spheres . Also called the hydrologic cycle. - PowerPoint PPT Presentation

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Page 1: Rivers and Streams

Rivers and Streams

Courtney MonroeFebruary 30, 2012

Page 2: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

Page 3: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

Also called the hydrologic cycle.

Page 4: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

Page 5: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

H2O can only be added to an area by runoff, by infiltration and by precipitation.

Page 6: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

H2O can only be removed from an area by runoff, by infiltration and by evaporation.

Page 7: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere, and other spheres.

H2O can only be removed from an area by runoff, by infiltration and by evaporation.

Transpiration (plants) and evaporation (from water areas) is called EVAPOTRANSPIRATION

Page 8: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere

Will the water budget ever be in balance locally?

Page 9: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere

Will the water budget ever be in balance locally?

NO!! It is usually raining, or transpiring/evaporating, but not both in equal amounts at the same time.

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Water Cycle ~ the movement of H2O through the hydrosphere

Will the water budget ever be in balance worldwide?

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Water Cycle ~ the movement of H2O through the hydrosphere

Will the water budget ever be in balance worldwide?

Yes!! Otherwise the air would “dry out”, or get “misty” everywhere.

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Water Cycle ~ the movement of H2O through the hydrosphere

Where will most of the water evaporate from?

Page 13: Rivers and Streams

Water Cycle ~ the movement of H2O through the hydrosphere

Where will most of the water evaporate from?

THE OCEAN, since ¾ of Earth is covered by it!!

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Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

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Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Page 16: Rivers and Streams

Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Infiltration ~ is water moving through the cracks and pores of surface soils.

Page 17: Rivers and Streams

Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Infiltration ~ is water moving through the cracks and pores of surface soils.

Transpiration ~ is the release of water from plants.

Page 18: Rivers and Streams

Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Infiltration ~ is water moving through the cracks and pores of surface soils.

Transpiration ~ is the release of water from plants.

Perspiration ~ is something that good athletes do a lot. Rarely seen at LSW????

Page 19: Rivers and Streams

Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Infiltration ~ is water moving through the cracks and pores of surface soils.

Transpiration ~ is the release of water from plants.

Perspiration ~ is something that good athletes do a lot. Rarely seen at LSW????

Evapotranspiration is a bit of both.

Page 20: Rivers and Streams

Water Cycle is water constantly moving among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth’s water supply is the water cycle.

Runoff ~ is water flowing downslope along the Earth’s surface.

Infiltration ~ is water moving through the cracks and pores of surface soils.

Transpiration ~ is the release of water from plants.

Perspiration ~ is something that good athletes do a lot. Rarely seen at LSW????

Evapotranspiration is a bit of both.

Recycling of water, almost does not exist. 90% of all water used by industry and cities runs back to the Ocean.

Page 21: Rivers and Streams

Runoff ~ water flowing down slope along the Earth’s surface.

Page 22: Rivers and Streams

Runoff ~ water flowing down slope along the Earth’s surface.

Page 23: Rivers and Streams

Factors that determine rates of water runoff

1. Amount of vegetation

Rate of Precipitation

Soil Composition

Slope

Page 24: Rivers and Streams

Factors that determine rates of water runoff

1. Amount of vegetation

2. Rate of Precipitation

Soil Composition

Slope

Page 25: Rivers and Streams

Factors that determine rates of water runoff

1. Amount of vegetation

2. Rate of Precipitation

3. Soil Composition

Slope

Page 26: Rivers and Streams

Factors that determine rates of water runoff

1. Amount of vegetation

2. Rate of Precipitation

3. Soil Composition

4. Slope

Page 27: Rivers and Streams

Factors that determine rates of water runoff

Amount of vegetation

Page 28: Rivers and Streams

Factors that determine rates of water runoff

Rate of precipitationhttp://waterdata.usgs.gov/ne/nwis/rt

Started to rain

Page 29: Rivers and Streams

Factors that determine rates of water runoff

Rate of precipitationhttp://waterdata.usgs.gov/ne/nwis/rt

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Page 31: Rivers and Streams
Page 32: Rivers and Streams

Factors that determine rates of water runoff

Soil composition. Loose soil with heavy rains, with little soil to hold it in place will often cause mud slides.

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Porosity is the amount of space in the pores of the soil, in this case a poorly sorted specimen.

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Permeability is how fast water will flow through something.

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Page 36: Rivers and Streams

Factors that determine rates of water runoff

Soil composition. Loose soil with heavy rains, with little soil to hold it in place will often cause mud slides.

Page 37: Rivers and Streams

Mud slide

Page 38: Rivers and Streams

Mud slide

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Mud slide

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Mud slide

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Factors that determine rates of water runoff

Slope

Page 44: Rivers and Streams

Stream Systems

Brooks and Creeks -> Streams

Streams --> Rivers

Rivers --> Watershed areas

Page 45: Rivers and Streams

Stream Systems

Brooks and Creeks -> Streams

Streams --> Rivers

Rivers --> Watershed areas

Brook behind Southwest High School

Salt Creek to

Platte River (French for “flat”)

Missouri

Mississippi

Gulf of Mexico

Ocean

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Continental Divide

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Stream Load ~ All the materials that the water in a stream carries.

Solution ~ Dissolved minerals.

Suspension ~ Particles held up by the moving water.

Bed load ~ Particles bounced along the bottom of the stream.

Page 49: Rivers and Streams

Stream Load ~ All the materials that the water in a stream carries.

Solution ~ Dissolved minerals.

a. Usually salts, or salt forming ions.

b. Counted in parts per million (ppm).

Page 50: Rivers and Streams

Stream Load ~ All the materials that the water in a stream carries.

Solution ~ Dissolved minerals. See page 216 in book.

Page 51: Rivers and Streams

Stream Load ~ All the materials that the water in a stream carries.

Suspension ~ Particles held up by the moving water.

Page 52: Rivers and Streams

Stream Load ~ All the materials that the water in a stream carries.

Bed load ~ Particles bounced along the bottom of the stream.

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Page 54: Rivers and Streams

Stream Velocity and Carrying Capacity

Stream Velocity based on how fast water flows.

Carrying capacity is how much of a stream load a stream can….carry.

Based largely on discharge.

m3/s = meters x meters x meters ÷ seconds

Page 55: Rivers and Streams

Floodplains

Flood ~ too much water in one place at one time.

Floodplain ~ where all that water goes

a. Nice an flat

b. Fertile soils

c. Sometimes covered with water

i 10 year flood

ii 50 year flood

iii 100 year flood

iv 500 year flood

Page 56: Rivers and Streams