Suspended load

The suspended load of a flow of fluid, such as a river, is the portion of its sediment uplifted by the fluid's flow in the process of sediment transportation. It is kept suspended by the fluid's turbulence. The suspended load generally consists of smaller particles, like clay, silt, and fine sands.

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4,841

Prior Five Years

1,152

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105,919

Prior Five Years

10,339

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7,653

Prior Five Years

5,988

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Academic Institutions Lifetime		Academic Institutions Prior Five Years		Non-academic Institutions Lifetime
#1	University of Queensland Australia	#1	Curtin University Australia	#1	United States Geological Survey United States
#2	University of Copenhagen Denmark	#2	West Virginia University United States	#2	National Oceanography Centre United Kingdom
#3	University of Exeter United Kingdom	#3	Ilia State University Georgia	#3	Rothamsted Research United Kingdom
#4	Ilia State University Georgia	#4	University of Illinois at Urbana-Champaign United States	#4	Environment and Climate Change Canada Canada
#5	University of Washington United States	#5	Asia University Taiwan	#5	Institut de Physique du Globe de Paris France
#6	University of Northern British Columbia Canada	#6	Beijing Normal University China
#7	Utrecht University Netherlands	#7	Cranfield University United Kingdom
#8	University of Toronto, Scarborough Canada	#8	Moscow State University Russia
#9	University of Lleida Spain	#9	University of Lincoln United Kingdom
#10	University of Tabriz Iran	#10	Cornell University United States
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