Sheet flow

Definition of Sheet flow: Sheet-flow sediment transport refers to transport of sandy sediments as a fluidized thin surface layer (thickness of ten to a few tens of grains). This is the common definition for Sheet flow, other definitions can be discussed in the article

Notes

Under strong wave action, transport in the sheet flow layer is the dominant transport mode: more important than bedload transport through saltation and rolling and more important than suspended load transport.

Sheet flow is a particular form of bedload sediment transport. Sheet flow transport occurs under strong wave action (wave orbital velocity greater than 1 m/s), where bed ripples are flattened out. In the sheet-flow layer, continuous contacts between sand grains create an intergranular stress. This stress decreases the velocity in the sheet-flow layer to about one half the velocity in the top layer. The sediment concentration in the sheet-flow layer is in the order of 100 to 1000 kg/m3.

See for further details Sediment transport formulas for the coastal environment#Sheet flow.

The main author of this article is Job Dronkers Please note that others may also have edited the contents of this article. Citation: Job Dronkers (2022): Sheet flow. Available from http://www.coastalwiki.org/wiki/Sheet_flow [accessed on 29-03-2023] For other articles by this author see Category:Articles by Job Dronkers For an overview of contributions by this author see Special:Contributions/Dronkers J