Flow structure and channel morphology after artificial chute cutoff at the meandering river in the upper Yellow River-Reference-Cited by-同舟云学术

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Flow structure and channel morphology after artificial chute cutoff at the meandering river in the upper Yellow River

Published:2022-01 Issue:2 Volume:15 Page:
ISSN:1866-7511
Container-title:Arabian Journal of Geosciences
language:en
Short-container-title:Arab J Geosci

Author:

Qiao Qiao,Li Chunguang^ORCID,Jing Hefang,Huang Lingxiao

Funder

national natural science foundation of china

key r & d plan projects of the science and technology department of ningxia autonomous region

ningxia science and technology department key research and development project

science research project of ningxia

special funds for fundamental research funds for central universities of northern university for nationalities

Natural Science Foundation of Ningxia

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

https://link.springer.com/content/pdf/10.1007/s12517-022-09431-6.pdf

Reference53 articles.

1. Allen JRL (1965) A review of the origin and characteristics of recent alluvial sediments. Sedimentology 5:89–191. https://doi.org/10.1111/j.1365-3091.1965.tb01561.x

2. Best JL, Rhoads BL (2008) Sediment transport, bed morphology and the sedimentology of river channel confluences. John Wiley & Sons, Ltd. 45-72. https://doi.org/10.1002/9780470760383.ch4

3. Biedenharn DS, Thorne CR, Watson CC (2000) Recent morphological evolution of the Lower Mississippi River. Geomorphology 34:227–249. https://doi.org/10.1016/s0169-555x(00)00011-8

4. Blanckaert K (2011) Hydrodynamic processes in sharp meander bends and their morphological implications. Journal of Geophysical Research-Earth Surface 116:1–22. https://doi.org/10.1029/2010JF001806

5. Constantine JA, Dunne T, Ahmed J, Legleiter C, Lazarus ED (2014) Sediment supply as a driver of river meandering and floodplain evolution in the Amazon Basin. Nat Geosci 7:899–903. https://doi.org/10.1038/ngeo2282

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