River Channel Processes defintions Flashcards
Erosion
Erosion is the continually shaping and wearing away of the bed and banks of the river channel by the power of water.
Hydraulic action
Is the force of the water pushing into cracks and hitting against the river’s banks.
The repeated action weakens the riverbank as air in the cracks is compressed and pressure builds up.
Collapsing air bubbles create small shock waves in a type of hydraulic action known as cavitation.
In rivers, hydraulics action is a low and ineffective process of erosion.
Corrasion/abrasion
Corrasion/abrasion - occurs when sediment in the river is thrown into or scraped along the banks of the riverbed.
This process is extremely common and is the main form of erosion within the river.
During times of high discharge the river has a greater capacity to transport larger material, which results in the greatest amount of damage.
Potholes may form as stones become trapped in depressions and hollows and are continually swirled around by eddies in the turbulent water.
Attrition
Is the process by which stones and sediment within the river become increasingly rounded. As material is transported it collides with other objects in the river. The collisions cause the stones to break into smaller pieces and the edges and points of the stones to break off.
Corrosion/solution
Corrosions/solution - is a continuous chemical process that occurs independently from river flow. Water that has slightly acidic properties. E.g. result of decomposing organic material (humic acid) or acid rain (carbonic acid), will chemically dissolve and weaken certain types of rock. Limestone is composed of calcium carbonate and is particularly vulnerable to corrosion.
Load transport
Is the movement of sediment by the river
Capacity
Is the total load of material actually transported
Competence
The maximum size of material that river is capable of transporting
Traction
Is when the largest stones, boulders and cobbles are rolled along the riverbed by strong turbulent currents
Saltation
Is where smaller bedload such as pebbles, stones and gravel are lifted and carried temporarily in the flow in a hopping or bouncing motion
Suspended load
Is when very fine particles of sand and silt are carried in suspension in fast flowing water.
Dissolved load/ solution
The process by which small dissolved sediments and minerals are transported within the river.
Critical erosion velocity
The lowest velocity at which sediment of a given size can be transported.
Deposition
Deposition is where the river drops its load when the river no longer has enough energy to carry the load. Deposition may occur when a river becomes shallower or when the volume of water decreases.