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Transports the eroded sediment downstream where it's deposited in the low velocity zone on the inside bank of the next meander. Such accumulations are called pointbar deposits. Meander inflections, or crossovers, often contain shallow riffles, particularly in gravel streams.A meander bend can become isolated when opposing cutbanks on a broadly looping meander intersect.
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Published December 2nd 2003 by Wildland Hydrology (first published October 1st 1996)
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Applied River Morphology Pdf Free
The terms river morphology and its synonym stream morphology are used to describe the shapes of riverchannels and how they change in shape and direction over time. The morphology of a river channel is a function of a number of processes and environmental conditions, including the composition and erodibility of the bed and banks (e.g., sand, clay, bedrock); erosion comes from the power and consistency of the current, and can effect the formation of the river's path. Also, vegetation and the rate of plant growth; the availability of sediment; the size and composition of the sediment moving through the channel; the rate of sediment transport through the channel and the rate of deposition on the floodplain, banks, bars, and bed; and regional aggradation or degradation due to subsidence or uplift. River morphology can also be effected by human interaction, which is a way the river responds to a new factor in how the river can change its course. An example of human induced change in river morphology is dam construction, which alters the ebb flow of fluvial water and sediment, therefore creating or shrinking estuarine channels.[1] A river regime is a dynamic equilibrium system, which is a way of classifying rivers into different categories. The four categories of river regimes are Sinuous canali- form rivers, Sinuous point bar rivers, Sinuous braided rivers, and Non-sinuous braided rivers.
Applied River Morphology Pdf Template
The study of river morphology is accomplished in the field of fluvialgeomorphology, the scientific term.
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See also[edit]
- Bedload, Suspended load
- Sediment, sedimentation, erosion
- River, Stream, Canal
- Water, Water resource
References[edit]
- ^Bo-yuan Zhu,Yi-tian Li,Yao Yue,Yun-ping Yang. Aggravation of north channels' shrinkage and south channels' development in the Yangtze Estuary under dam-induced runoff discharge flattening. Journal Estuarine, Coastal and Shelf Science. 5 March 2017
- Rosgen, Dave (1996). Applied River Morphology. 2nd ed. (Fort Collins, CO: Wildland Hydrology, publ.) ISBN978-0-9653289-0-6.
- Brice J C. Planform properties of meandering rivers [C].River Meandering, Proceedings of the October 24–26, 1983 Rivers '83 Conference, ASCE. New Orleans, Louisi- ana, 1983. 1-15.
External links[edit]
Applied River Morphology Pdf Example
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