Movie:Bed load sediment transport close up: Difference between revisions
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Watermann1 (talk | contribs) (Created page with '{{Upload movie |Movie type=Laboratory |Upload image movie=Bedload_close.jpg }} {{Attribute movie1 |Movie domain=terrestrial }} {{Attribute movie3}} {{Movie description |Grade lev…') |
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{{Upload movie | {{Upload movie | ||
|Movie type=Laboratory | |Movie type=Laboratory | ||
|Upload movie=pZpC10fE3fg | |||
|Upload image movie=Bedload_close.jpg | |Upload image movie=Bedload_close.jpg | ||
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|Movie domain=terrestrial | |Movie domain=terrestrial | ||
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|Movie keywords=bed load | |||
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{{Attribute movie2 | |||
|Movie keywords=transportation | |||
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{{Attribute movie3 | |||
|First name contributor=Chris | |||
|Last name contributor=Paola | |||
|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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Grain Size ratio = 35 | Grain Size ratio = 35 | ||
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{{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}} | {{Movie references2}} | ||
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Latest revision as of 15:17, 21 June 2017
Information Page: Bed load sediment transport close up
Play Laboratory
Key Attributes
| Domain: | terrestrial |
| Keywords: | bed load |
| Keywords: | transportation |
| Model name: | Animation model name |
| Name: | Chris, Paola |
| Where: | - |
| When: | - |
Short Description
Grade level: High (9-12), Under graduate (13-16)
Statement: Bed load transportation
Abstract: A close up of bed load transportation with a still camera frame. 50g/m/s 7.0mm d50 50g/m/s 0.20mm d50 Grain Size ratio = 35
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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