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Statements

Subject Item
dbr:Bed_material_load
rdfs:label
Bed material load ベッドマテリアルロード
rdfs:comment
ベッドマテリアルロード(英語:bed material load)は、主として河床に有意に存在する砂礫からなり、河床を構成する砂礫と交換を繰り返す流砂である。 この流砂は、河床高、河床形態、河床の粒度分布を変化させる。 Three components that are included in the load of a river system are the following: dissolved load, wash load and bed material load. The bed material load is the portion of the sediment that is transported by a stream that contains material derived from the bed. Bed material load typically consists of all of the bed load, and the proportion of the suspended load that is represented in the bed sediments. It generally consists of grains coarser than 0.062 mm with the principal source being the channel bed. Its importance lies in that its composition is that of the bed, and the material in transport can therefore be actively interchanged with the bed. For this reason, bed material load exerts a control on river channel morphology. Bed load and wash load (the sediment that rides high in the fl
dct:subject
dbc:Geomorphology dbc:Sedimentology
dbo:wikiPageID
23993216
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1045189296
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dbr:Bed_load dbc:Sedimentology dbr:River_bed dbr:Sediment_transport dbr:Suspended_load dbr:Dissolved_load dbr:Wash_load dbr:Sediment dbc:Geomorphology
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dbpedia-ja:ベッドマテリアルロード n11:4053404-2 wikidata:Q26920631 n14:2X1Eg freebase:m.07kh2fq
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dbt:Reflist dbt:Sediment_transport dbt:Rivers,_streams_and_springs
dbo:abstract
ベッドマテリアルロード(英語:bed material load)は、主として河床に有意に存在する砂礫からなり、河床を構成する砂礫と交換を繰り返す流砂である。 この流砂は、河床高、河床形態、河床の粒度分布を変化させる。 Three components that are included in the load of a river system are the following: dissolved load, wash load and bed material load. The bed material load is the portion of the sediment that is transported by a stream that contains material derived from the bed. Bed material load typically consists of all of the bed load, and the proportion of the suspended load that is represented in the bed sediments. It generally consists of grains coarser than 0.062 mm with the principal source being the channel bed. Its importance lies in that its composition is that of the bed, and the material in transport can therefore be actively interchanged with the bed. For this reason, bed material load exerts a control on river channel morphology. Bed load and wash load (the sediment that rides high in the flow and does not extract non-negligible momentum from it) together constitute the total load of sediment in a stream. The order in which the three components of load have been considered – dissolved, wash, bed material – can be thought of as progression: of increasingly slower transport velocities, so that the load peak lags further and further behind the flow peak during any event.
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wikipedia-en:Bed_material_load?oldid=1045189296&ns=0
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8586
foaf:isPrimaryTopicOf
wikipedia-en:Bed_material_load