Experimental study of the effect of grain sizes in a bimodal mixture on bed slope, bed texture, and the transition to washload-Reference-Cited by-同舟云学术

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Experimental study of the effect of grain sizes in a bimodal mixture on bed slope, bed texture, and the transition to washload

Published:2017-01 Issue:1 Volume:53 Page:923-941
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Hill Kimberly M.¹²^ORCID,Gaffney John³^ORCID,Baumgardner Sarah¹⁴,Wilcock Peter⁵,Paola Chris¹⁴^ORCID

Affiliation:

1. St. Anthony Falls LaboratoryUniversity of MinnesotaMinneapolis Minnesota USA

2. Department of Civil, Environmental, and Geo‐EngineeringUniversity of MinnesotaMinneapolis Minnesota USA

3. Inter‐Fluve, Inc.Hood River Oregon USA

4. Department of Earth SciencesUniversity of MinnesotaMinneapolis Minnesota USA

5. Department of Watershed SciencesUtah State UniversityLogan Utah USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016WR019172

Reference67 articles.

1. Framework dilation, winnowing, and matrix particle size; the behavior of some sand-gravel mixtures in a laboratory flume

2. STUDY ON HYDRAULIC RESISTANCE AND BED-LOAD TRANSPORT RATE IN ALLUVIAL STREAMS

3. The effects of kinetic sorting on sediment mobility on steep slopes

4. The combined use of wash load and bed material load rating curves for the calculation of total load: An example from the Burdekin River, Australia

5. The Intrusion of Fine Sediments into a Stable Gravel Bed

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1. The roles of geometry and viscosity in the mobilization of coarse sediment by finer sediment;Proceedings of the National Academy of Sciences;2024-09-12

2. Autogenic Formation of Bimodal Grain Size Distributions in Rivers and Its Contribution to Gravel‐Sand Transitions;Geophysical Research Letters;2024-09-02

3. Fine Sediment in Mixed Sand‐Silt Environments Impacts Bedform Geometry by Altering Sediment Mobility;Water Resources Research;2024-07

4. Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics;Earth Surface Dynamics;2024-02-15

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