The bed load of the River Severn typically consists of a mix of sediment types, including gravel, sand, and pebbles, which can vary in size from small grains to larger stones. The shape of these particles is often rounded or sub-rounded due to the processes of erosion and transport along the riverbed. The specific size and shape can change depending on the location within the river and the energy of the water flow, with coarser materials generally found in faster-flowing sections.
The size of the pebble will decrease down stream because the further downstream you go the quicker the river velocity. This means there will be more abrasion against the sides and bed of the river and the friction will be greater, this wears away the river load making it decrease in size. Increase velocity means that bigger material will be picked up by the river and carried as river load. More load in the river and increased size of load will mean more attrition and the river load will keep colliding into each other smoothening and rounding their shape. Brap brap !!
The amount of sediments a river can carry is influenced by factors such as the river's velocity, volume of water, slope of the river bed, sediment particle size, and the presence of vegetation or structures that can trap sediments. Increased velocity and water volume typically result in higher sediment transport capacity.
it would be the size of the river's headwatersC: Size of the river's head watersTemperature of the river
The size of the pebble will decrease down stream because the further downstream you go the quicker the river velocity. This means there will be more abrasion against the sides and bed of the river and the friction will be greater, this wears away the river load making it decrease in size. Increase velocity means that bigger material will be picked up by the river and carried as river load. More load in the river and increased size of load will mean more attrition and the river load will keep colliding into each other smoothening and rounding their shape. Brap brap !!
Faster river velocities are capable of carrying greater amounts of bedload and transporting them farther and faster. The shape of the sediments of the bedload would therefore be exposed to more physical weathering which would progressively round the sediments and also decrease their size.
the gradient of the slope The channel roughness The amount and size of bed load
what is bed load particle size
Factors includesThe weight of the load lifted· The range of the lift· The location of the load in relation to the body· The size and shape of the load· Distance and duration the load is carried· The number and frequency of lifts performed
To find river bedload, you can collect sediment samples from the river bed and analyze them in a laboratory. Another method is to use a sediment trap or gauge to measure the amount of sediment transported by the river over time. This can help determine the size and composition of the bedload in the river.
The size of load material affects river transportation because larger materials, like boulders and gravel, require more energy and force to be moved, which typically occurs in higher flow velocities during floods or fast-moving currents. Smaller particles, such as sand and silt, can be easily lifted and carried by lower energy flows, allowing them to be transported over longer distances. Additionally, the size influences how materials interact with the riverbed and each other, affecting erosion, sediment deposition, and overall river morphology. Thus, the transport dynamics differ significantly based on the load size.
The load in a river can be transported in 4 ways. The first is Traction. It is when rocks and boulders are rolled along the river bed by the force of the water. The second is Saltation this is when stones and pebbles are bounced along the river bed. The third is Suspension this is when fine particles like silt floot along in the water. The last is Solution which is when the material dissolves in the water. These different methods are used depending on the size of the load to be transported and the energy of the river. A river needs little energy to transport a small mineral by solution but lots of energy to transport heavy boulders it by traction.
This is the amount of load a river can carry. Generally, the load quantity will increase with discharge and velocity because rivers of higher discharge and velocity have more energy so will be able to carry more load. Therefore, load quantity increases downstream. Also, small particles require less energy to be carried so as the load size decreases, quantity increases