Difference between revisions of "Bedload"
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Tasomerville (talk | contribs) (New page: {{ Definition|title=Bedload |definition= Sediment transport mode in which individual particles either roll or slighe along the seabed as a shallow, mobile layer a few particle diameters de...) |
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Definition|title=Bedload | Definition|title=Bedload | ||
| − | |definition= Sediment transport mode in which individual particles either roll or | + | |definition= Sediment transport mode in which individual particles either roll or slide along the seabed as a shallow, mobile layer a few particle diameters deep.<ref name="CIRIA (1996)"> CIRIA (1996). ''Beach management manual''. CIRIA Report 153.</ref>.}} |
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| + | Bedload transport is the dominant sediment transport mode when the flow velocities (currents and wave-orbital velocities) are above the critical velocity for setting bed particles in motion (in the order of 0.2-0.4 m/s for sandy sediments), but insufficient for bringing sediment particles in suspension. Bedload transport occurs for non-cohesive medium-coarse sediments and is associated with the formation of bed ripples and dunes. The migration of these bedforms yields an estimate for the bedload transport. | ||
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==See also== | ==See also== | ||
| + | :[[Sand transport]] | ||
| + | :[[Coastal Hydrodynamics And Transport Processes]] | ||
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| + | ==References== | ||
| + | <references/> | ||
Latest revision as of 12:04, 27 March 2021
Definition of Bedload:
Sediment transport mode in which individual particles either roll or slide along the seabed as a shallow, mobile layer a few particle diameters deep.[1].
This is the common definition for Bedload, other definitions can be discussed in the article
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Bedload transport is the dominant sediment transport mode when the flow velocities (currents and wave-orbital velocities) are above the critical velocity for setting bed particles in motion (in the order of 0.2-0.4 m/s for sandy sediments), but insufficient for bringing sediment particles in suspension. Bedload transport occurs for non-cohesive medium-coarse sediments and is associated with the formation of bed ripples and dunes. The migration of these bedforms yields an estimate for the bedload transport.
See also
References
- ↑ CIRIA (1996). Beach management manual. CIRIA Report 153.
