Abstract. We measured a wide range of transport rates for five different sand/gravel mixtures in a laboratory flume. Each mixture used the same gravel, and sand was added to produce mixtures containing 6, 15, 21, 27, and 34 % sand. Control of other variables allows us to isolate the effect of bed sand content on transport. As sand content increases, gravel transport rates increase by orders of magnitude, even though the proportion of gravel in the bed decreases. The increase in gravel transport rate is most rapid over the range of bed sand content between 15 and 27%. The increase in transport rate is larger than predicted using standard scaling relations between transport rate and grain size, indicating that models of transport and sorting ...
The movement of individual clasts over a water-lain gravel substrate is investigated in a series of ...
In a river channel the prevailing bedload transport rate is not solely independent upon hydraulic pa...
This study consists of three sections: - experiments on sand transport in oscillatory sheet flow wit...
Abstract. We measured a wide range of transport rates for five different sand/gravel mixtures in a l...
We measured a wide range of transport rates for five different sand/gravel mixtures in a laboratory ...
Experiments were conducted in a laboratory flume channel to evaluate the effects of increasing amoun...
In a series of flume experiments using constant discharge, flow depth, and gravel feed rate, sand fe...
A flume experiment was conducted to examine the evolution of a sand-gravel reach under a lack of sed...
Fine-grained sediment represents a significant component of the total transport load in most fluvial...
We present a transport model for mixed sand/gravel sediments. Fractional transport rates are referen...
Measurements in a braided reach of the proglacial White River, Washington, are used to compare the b...
[1] A mixed-size sediment transport model using only two fractions, sand and gravel, offers practica...
A mixed-size sediment transport model using only two fractions, sand and gravel, offers practical ad...
New experiments with graded sand were conducted in the large oscillating tunnel of Delft Hydraulics....
International audienceA reliable estimation of sediment transport in gravel-bed streams is important...
The movement of individual clasts over a water-lain gravel substrate is investigated in a series of ...
In a river channel the prevailing bedload transport rate is not solely independent upon hydraulic pa...
This study consists of three sections: - experiments on sand transport in oscillatory sheet flow wit...
Abstract. We measured a wide range of transport rates for five different sand/gravel mixtures in a l...
We measured a wide range of transport rates for five different sand/gravel mixtures in a laboratory ...
Experiments were conducted in a laboratory flume channel to evaluate the effects of increasing amoun...
In a series of flume experiments using constant discharge, flow depth, and gravel feed rate, sand fe...
A flume experiment was conducted to examine the evolution of a sand-gravel reach under a lack of sed...
Fine-grained sediment represents a significant component of the total transport load in most fluvial...
We present a transport model for mixed sand/gravel sediments. Fractional transport rates are referen...
Measurements in a braided reach of the proglacial White River, Washington, are used to compare the b...
[1] A mixed-size sediment transport model using only two fractions, sand and gravel, offers practica...
A mixed-size sediment transport model using only two fractions, sand and gravel, offers practical ad...
New experiments with graded sand were conducted in the large oscillating tunnel of Delft Hydraulics....
International audienceA reliable estimation of sediment transport in gravel-bed streams is important...
The movement of individual clasts over a water-lain gravel substrate is investigated in a series of ...
In a river channel the prevailing bedload transport rate is not solely independent upon hydraulic pa...
This study consists of three sections: - experiments on sand transport in oscillatory sheet flow wit...