The Origin of Fine Sediment Determines the Observations of Suspended Sediment Fluxes Under Unsteady Flow Conditions-Reference-Cited by-同舟云学术

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The Origin of Fine Sediment Determines the Observations of Suspended Sediment Fluxes Under Unsteady Flow Conditions

Published:2018-08 Issue:8 Volume:54 Page:5654-5669
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Juez Carmelo¹^ORCID,Hassan Marwan A.²^ORCID,Franca Mário J.³^ORCID

Affiliation:

1. Laboratoire de Constructions HydrauliquesÉcole Polytechnique Fédérale de Lausanne Lausanne Switzerland

2. Department of GeographyThe University of British Columbia Vancouver Canada

3. Water Science and Engineering DepartmentIHE‐Delft Institute for Water Education Delft Netherlands

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018WR022982

Reference50 articles.

1. Experimental study of sediment transport hysteresis

2. Suspended sediment dynamics in a large drainage basin: the River Rhine

3. Fitting and interpretation of sediment rating curves

4. Hysteresis effect in suspended sediment concentration in the Rybárik basin, Slovakia / Effet d'hystérèse dans la concentration des sédiments en suspension dans le bassin versant de Rybárik (Slovaquie)

5. Reservoir-induced hydrological changes in the Ebro River basin (NE Spain)

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