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.
load
material that a river carries along E.g (stone, grass & rocks)
clay.
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.
The velocity and discharge volume of the stream or river.
the gradient of the slope The channel roughness The amount and size of bed load
It is called suspension.
The total sediment load transported by a stream is the sum of the bed load, suspended load, and dissolved load. Bed load consists of larger particles that roll, slide, and bounce along the streambed. Suspended load is finer particles carried in the water column, while dissolved load is material that is dissolved in the water itself.
Moving water in a river can pick up sediment and carry it along in a suspended load. This includes small particles like silt and clay that are held up and transported within the flow of the water.
Stream Load is the amount of material a stream can hold as it flows. As a stream flows it causes erosion, and this erosion is carried about as material in the stream. As too much is eroded, the extra material will fall to the bottom, or push it's way to the sides.
Suspended load: All organic and inorganic material carried in moving water Dissolved load: All organic and inorganic material carried in solution by moving water Bed load: Coarse materials such as gravel, stones. These things move along the bottom of the river by rolling, or sliding.
Geologists commonly us the term STREAM for any body of water that flows in a channel.TOTAL LOADRivers move not only water but also a tremendous amount of material. This material, called the total load, consists of bed load, suspended load and dissolved load. Bed loadcomprises particles of sand and gravel that slide, roll, and bounce along the channel bottom in rapidly moving water. Suspended load comprises mainly silt and clay particles carried in suspension above the riverbed. Dissolved load comprises electrically charged atoms or molecules, called ions, that are carried in solution in the water