Movie:Sheet flow bedload movement: Difference between revisions

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{{Upload movie
{{Upload movie
|Movie type=Laboratory
|Movie type=Laboratory
|Upload movie=Rte-booksheetpeng(new).avi
|Upload movie=vpDHDAK53A8
|Upload image movie=Sheetpeng.jpg
|Upload image movie=Sheetpeng.jpg
|Caption movie=Sheet flow bedload movement
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{{Attribute movie1
{{Attribute movie1
|Movie domain=terrestrial
|Movie domain=terrestrial
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{{Attribute movie3}}
{{Attribute movie2
|Movie keywords=bed load
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{{Attribute movie2
|Movie keywords=sheet flow
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{{Attribute movie3
|First name contributor=Gary
|Last name contributor=Parker
|Location movie=--
|Timespan movie=--
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{{Movie description
{{Movie description
|Grade level=High (9-12), Under graduate (13-16)
|Grade level=High (9-12), Under graduate (13-16)
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|Extended movie description=Sheet flow style bed load transportation with colored marker stones.  In this form of bed load transport a portion of the bed moves as a unified sheet.
|Extended movie description=Sheet flow style bed load transportation with colored marker stones.  In this form of bed load transport a portion of the bed moves as a unified sheet.
}}
}}
{{Movie theory2}}
{{Movie theory2
|Theory movie=Bed load transportation is a function of the fluid force per area, or shear stress on the stream bed.  Shear stress is proportional to the specific weight of the fluid, the depth and the surface slope of the fluid.  The frictional resisting force is proportional  to the specific weight of the sediment and the diameter of the sediment.
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{{Movie references2}}
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Latest revision as of 16:33, 21 June 2017

Information Page: Sheet flow bedload movement

Play Laboratory


Sheet flow bedload movement



Key Attributes

Domain: terrestrial
Keywords: bed load
Keywords: sheet flow
Model name: Animation model name
Name: Gary, Parker
Where: --
When: --


Short Description

Grade level: High (9-12), Under graduate (13-16)

Statement: Sheet Flow

Abstract: Sheet flow style bed load transportation with colored marker stones. In this form of bed load transport a portion of the bed moves as a unified sheet.

Theory

Bed load transportation is a function of the fluid force per area, or shear stress on the stream bed. Shear stress is proportional to the specific weight of the fluid, the depth and the surface slope of the fluid. The frictional resisting force is proportional to the specific weight of the sediment and the diameter of the sediment.

Links

References



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