Movie:Sheet flow bedload movement: Difference between revisions
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{{Attribute movie1 | {{Attribute movie1 | ||
|Movie domain = terrestrial | |Movie domain=terrestrial | ||
}} | }} | ||
{{Attribute movie2 | {{Attribute movie2 | ||
|Movie keywords = bed load | |Movie keywords=bed load | ||
}} | }} | ||
{{Attribute movie2 | {{Attribute movie2 | ||
|Movie keywords = sheet flow | |Movie keywords=sheet flow | ||
}} | }} | ||
{{Attribute movie3 | {{Attribute movie3 | ||
|First name contributor=Gary | |First name contributor=Gary | ||
|Last name contributor =Parker | |Last name contributor=Parker | ||
|Location movie=-- | |Location movie=-- | ||
|Timespan 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) | ||
|One-line movie description = Sheet Flow | |One-line movie description=Sheet Flow | ||
|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. | ||
}} | }} | ||
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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