Journal of Geophysical Research Atmospheres · 2010 · 107 citations · 25 references
Natural ResourcesEarth SciencesHydrologySediment TransportSedimentologyStream RestorationBed Load TransportFluvial Sediment TransportGrain Size DistributionSediment DepositionSediment FluxSediment Transport In RiversBed Material LoadBedload Grain Size DistributionCoarse Sediment DepositionFluvial Sediment Grain SizeGrain-size Effects On TransportGravel-bed RiversSediment Grain-size DistributionSediment Pulses
Sediment supply to gravel bed river channels often takes the form of episodic sediment pulses, and there is considerable interest in introducing sediment pulses in stream restorations to alter bed surface grain size distributions and bed mobility. A series of laboratory experiments was conducted in order to examine how sediment pulse grain size and volume affects the mobility of bed material in gravel bed channels. Pulses used in the experiments were composed of either the fine tail or the median of the subsurface bed material grain size distribution. Bed material refers to sediment in the channel prior to the pulse introduction exclusively. Both types of pulse were finer than the bed material surface median. Two pulse sizes were used, which were either equivalent to the volume of sediment required to cover the entire bed one median subsurface bed material grain diameter deep (full unit) or 1/4 of this volume (1/4 unit). The latter was designed to produce a transitory pulse. With the exception of the 1/4 unit coarse pulse, introduction of the sediment pulses to the channel caused dramatic increases in the bed load flux. The coarse sediment pulses fine the bed surface and coarsen the bed load. Finer pulses also fine the surface, but the bed load fines while the bed material load (that excludes pulse material) coarsens. The greatest effects on the fractional transport occurred during the full unit fine pulse where the pulse covered the greatest bed surface and effectively smoothed the bed, increasing near bed velocity and mobilizing the coarse particles. Overall, the coarse pulses were not very effective at mobilizing bed material. The large fine pulse mobilized ∼35% of the bed material surface (∼35% of its input weight) and was most effective at mobilizing the surface. However, the small fine pulse mobilized 50% of its input weight as it passed through the channel, making it the most efficient at mobilizing the bed material.
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Threshold of sediment motion under unidirectional currents
Martin C. Miller, I Nick McCave, Paul D. Komar · Sedimentology · 1977 · 980 citations
Sediment supply and the development of the coarse surface layer in gravel-bedded rivers
W. E. Dietrich, James W. Kirchner, Hiroshi Ikeda et al. · Nature · 1989 · 690 citations
On why gravel bed streams are paved
Gary Parker, Peter C. Klingeman · Water Resources Research · 1982 · 608 citations