Riverbed structures, which affect bed load transportation in mountain streams, are structures of boulders and cobbles on mountain streambed rearranged by flood flow to reach high resistance and high bed stability. A parameter Sp was introduced to describe the intensity of a riverbed structure. A specially designed instrument was used to measure the riverbed structure intensity, and a double-box bed load sampler was used to measure the transport rate of bed load. Field measurements on the bed load transportation, riverbed structure and hydraulic features were conducted in 15 tributaries of Xiaojiang River in the upper Yangtze River Basin in China. It has been found that the transport rate of bed load is affected by both the unit stream power...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
The influence of vegetation upon bedload transport and channel morphodynamics is examined along a ch...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
Field experiments were conducted on bed load transport in the Diaoga River, a mountain stream in sou...
Bed load transport in mountain streams is closely linked to streambed structures. Strambed structure...
Bed load transport in mountain streams is very difficult to be determined since it strongly correlat...
AbstractBed structures in many mountain rivers provide additional resistance to the flow. A field ex...
Flood discharge and sediment transport are closely linked to channel resistance in steep mountain st...
Streambed structures have developed in many mountain rivers as a result of fluvial morphology. They ...
Rivers and streams with the flow, sediment, and habitat seasonality are termed as intermittent river...
Although sediment transport in the uppermost parts of mountain basins may be supply- limited, bedloa...
We monitor bedload transport and water discharge at six stations in two forested headwater streams o...
Developing a bed load transport for size fractions requires an understanding of basic theory for the...
A 14-month continuous record of the spatial variation in the incidence and magnitude of bed load tra...
The prediction and calculation of the volume of gravel and/or sand transported down streams and rive...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
The influence of vegetation upon bedload transport and channel morphodynamics is examined along a ch...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
Field experiments were conducted on bed load transport in the Diaoga River, a mountain stream in sou...
Bed load transport in mountain streams is closely linked to streambed structures. Strambed structure...
Bed load transport in mountain streams is very difficult to be determined since it strongly correlat...
AbstractBed structures in many mountain rivers provide additional resistance to the flow. A field ex...
Flood discharge and sediment transport are closely linked to channel resistance in steep mountain st...
Streambed structures have developed in many mountain rivers as a result of fluvial morphology. They ...
Rivers and streams with the flow, sediment, and habitat seasonality are termed as intermittent river...
Although sediment transport in the uppermost parts of mountain basins may be supply- limited, bedloa...
We monitor bedload transport and water discharge at six stations in two forested headwater streams o...
Developing a bed load transport for size fractions requires an understanding of basic theory for the...
A 14-month continuous record of the spatial variation in the incidence and magnitude of bed load tra...
The prediction and calculation of the volume of gravel and/or sand transported down streams and rive...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
The influence of vegetation upon bedload transport and channel morphodynamics is examined along a ch...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...