Abstract
Natural streambed does not exhibit a flat bed surface but takes various geometrical forms known as bedforms. In this chapter, the experimental and theoretical studies dealing with the formation, geometry, and stability of bedforms are furnished. The predictors of various bedforms are discussed in details. Bedforms in gravel-bed streams are given. The important feature of this chapter is the presentation of mathematical models proposed by various researchers. Further, the resistance to flow due to bedforms is of paramount importance to river engineers. This issue is also discussed. Numerical examples on bedforms are given in the end of the chapter.
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Notes
- 1.
In terms of Shields parameter, ripples can occur at about Θ = 10–14Θc, where Θ and Θc are the Shields parameter and the threshold Shields parameter, respectively. The Shields parameter is defined as Θ = τ 0/(Δρgd), and the threshold Shields parameter Θc corresponds to the threshold bed shear stress τ 0c. Here, τ 0 is the bed shear stress \( ( = \rho u_{*}^{2} ) \), Δ is the submerged relative density (= s − 1), s is the relative density of sediment (= ρ s/ρ), ρ s is the mass density of sediment, ρ is the mass density of water, g is the acceleration due to gravity, and d is the median particle size.
- 2.
The Kelvin–Helmholtz instability may occur when there is shear at the interface between two flowing fluids.
- 3.
Biunivocal is a type of relationship that exclusively links two terms to one another on the basis of one of the two terms.
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Dey, S. (2014). Bedforms. In: Fluvial Hydrodynamics. GeoPlanet: Earth and Planetary Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-19062-9_8
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