UNSTEADY 1D FLOW MODEL OF COMPOUND CHANNEL WITH VEGETATED FLOODPLAINS

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dc.contributor.author Helmio T.
dc.date.accessioned 2021-05-04T05:49:30Z
dc.date.available 2021-05-04T05:49:30Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=1264682
dc.identifier.citation Journal of Hydrology, 2002, 269, 1-2, 89-99
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/28373
dc.description.abstract In areas that are occasionally inundated by floods, it is essential to know the quantity and density of vegetation that can be allowed while avoiding flooding beyond the intended floodplains. An unsteady flow model was developed for a channel with vegetated floodplains, to take into account the retention effects of the vegetated areas on flood wave conveyance. A one-dimensional (1D) unsteady flow model was combined with Nuding's method, which takes into account the friction caused by vegetation and the additional resistance caused by the interaction between the main channel and vegetated areas. Nuding's method was used to compute the total Darcy-Weisbach friction factor for each cross section and each water level as input data for each time step of the flow model. The model was applied to a double-trapezoidal channel, and the results were compared with a traditional model, in which floodplains were considered only as storage. Differences in the conveyance capacity of the channel were found between the models.
dc.subject HYDRAULICS
dc.subject RIVERS
dc.subject FLOODPLAINS
dc.subject VEGETATION
dc.subject ROUGHNESS
dc.title UNSTEADY 1D FLOW MODEL OF COMPOUND CHANNEL WITH VEGETATED FLOODPLAINS
dc.type Статья


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