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Journal ArticleDOI

Patterns of alluvial rivers

Stanley A. Schumm
- 01 Jan 1985 - 
- Vol. 13, Iss: 1, pp 5-27
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TLDR
A review of alluvial river patterns can be found in this article, where the authors discuss the relationship between hydrology, hydraulics, geology, and geomorphology at all scales.
Abstract
The pattern (planform) of a river can be considered at vastly different scales, depending upon both the size of the river and the part of the fluvial system that is under consideration (Figure 1). For example, in the broadest sense, river patterns comprise a drainage network (dendritic, parallel, trellis, etc; Figure lA). The type of pattern is of interest to geomorphologists and geologists who interpret geologic conditions from aerial photographs. At another scale a river reach (which in Figure lB is meandering) is of interest to the geomorphologist who is interested in what that pattern reveals about river history and behavior, and to the engineer who is charged with maintaining navigation and preventing major instability. When a single meander is examined (Figure 1 C), the hydraulics offtow, the sediment transport, and the potential for bank erosion are of concern. In addition, the sedimentologist is interested in the distribution of sediment within the bend, bed forms within the channel (Figure lD), and sedimentary structures (Figure IE), which also establish a component of roughness for the hydraulic engineer. Finally, the individual grains (Figure IF) provide geologic information on the sediment sources, the nature of sediment loads, and the feasibility of dredging for gravel. There is an interaction of hydrology, hydraulics, geology, and geomorphology at all scales, which emphasizes the point that the fluvial system as a whole cannot be ignored, even though only a component of the system is to be studied. In this review only the patterns or planforms of alluvial rivers are discussed, although it is apparent that the hydrologic and sediment yield characteristics of the drainage basin (Figure lA), as well as its geologic history, cannot be ignored in the explanation of the pattern of any river

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Citations
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Journal ArticleDOI

Ecological connectivity in alluvial river ecosystems and its disruption by flow regulation

TL;DR: The dynamic nature of alluvial floodplain rivers is a function of flow and sediment regimes interacting with the physiographic features and vegetation cover of the landscape as discussed by the authors, and restoration efforts should focus on reestablishing dynamic connectivity between the channel and floodplain water bodies.
Journal ArticleDOI

Riverine landscapes: biodiversity patterns, disturbance regimes, and aquatic conservation

J.V. Ward
TL;DR: To be effective, conservation efforts should be based on a solid conceptual foundation and a holistic understanding of natural river ecosystems, and background knowledge is necessary to re-establish environmental gradients, to reconnect interactive pathways, and to reconstitute some semblance of the natural dynamics responsible for high levels of biodiversity.
Journal ArticleDOI

Anabranching rivers: their cause, character and classification

TL;DR: Anabranching rivers as mentioned in this paper consist of multiple channels separated by vegetated semi-permanent alluvial islands excised from existing floodplain or formed by within-channel or deltaic accretion.
Journal ArticleDOI

Bed material transport and the morphology of alluvial river channels

TL;DR: In this article, the authors studied the relationship between sediment transport and river morphology by defining sediment transport regimes on the basis of the Shields number, a non-dimensional measure of the capacity of the channel to move sediment of a given caliber.
Journal ArticleDOI

The serial discontinuity concept : extending the model to floodplain rivers

TL;DR: In this article, the authors consider the dynamics of alluvial flood plain rivers using a three reach characterization: constrained headwater reach, braided reach, and meandering reach.
References
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Book

The fluvial system

Journal ArticleDOI

Experimental Study of Channel Patterns

TL;DR: In this paper, a series of experiments were performed in a large flume to determine the effect of slope and sediment load on channel patterns, and the results indicated that landforms may not always respond progressively to altered conditions and dramatic morphologic changes can occur abruptly when critical erosional and (or) depositional threshold values are exceeded.
Book

Rivers: Form and Process in Alluvial Channels

TL;DR: In this article, a detailed review of alluvial river form and process is presented, focusing on the environmental catchment factors that control the development of channel equilibrium, and a detailed analysis of the channel equilibrium process is provided.