Long Profile/Channel Characteristics Flashcards
what does the long profile show
how the gradient of the river channel changes form the rivers source to its mouth by showing the height of the river bed above the base level for the whole length of the river
what is the base level
the lowest point that the river can erode to - usually sea level
when, generally, to landforms such as waterfalls occur - and how does this affect the profile of the river
when the rates of erosion and deposition change along the course of a river
It makes the profile uneven
what is balanced along the course of a river
total amount of erosion and deposition
what is a graded profile, and when does it occur
when over time the long profile goes from being uneven to being a curve.
occurs as the total amount of deposition and erosion is balanced, and the rate of erosion of landforms like waterfalls is equal to the rate of deposition elsewhere along the river
describe the upper stage of the river
- steep gradient
- river is high above sea level
- this gives it a lot of potential energy
describe the middle stage of the river
- as gradient decreases, potential energy is converted to kinetic energy - the river gains velocity
describe the lower stage of the river
little potential energy
lots of kinetic energy
highest velocity
what increases downstream as you move from source to mouth
velocity
discharge
why does discharge increase downstream
tributaries (smaller streams and rivers) and more surface runoff join the main channel
what is river velocity influenced by
gradient, discharge and channel characteristics (shape and roughness)
what will an efficient river have
high velocity, high discharge and little friction
how is efficiency measured
hydraulic radius
- larger HR means more efficient
what is the hydraulic radius
channels cross section area divided by length of its wetted perimeter
- contact between water and wetted perimeter creates frictions,which increases energy loss and slows the river down
- larger hydraulic radius means smaller proportion of water is in contact with the wetted perimeter. So friction is lower, which reduces energy loss,increasing velocity and discharge
- smooth, narrow, deep channels have larger HR
how does channel roughness affect efficiency
large angular boulders/protruding banks increase wetted perimeter and cause more frictions. reduces E,V,D
what happens when channel roughness increases
so does turbulence
causes greater erosion
what happens when channel roughness increases
so does turbulence
causes greater erosion as turbulent flow is more effective at picking up particles from the river bed
explain channel roughness in the upper/lower stages
- greatest in the upper stages. altho gradient is steep, the river loses a lot of energy to friction, so discharge and velocity are lowest here during normal conditions
- in the lower stages, the banks and bed of the river are smooth, so theres much less friction. this means less energy is lost, so discharge and velocity are the highest in this stage
what is erosion like in the upper stage
- mainly vertical and by abrasion (some hydraulic action)
- erosion occurs when there are high energy conditions (i.e when velocity and discharge are high after heavy rain/ice melt
- rough channel causes turbulence and the large angular bedload is dragged along the river bed causing intense downward erosion
what is transportation like in the upper stage
- mainly large particles such as boulders carried by traction or saltation during high energy conditions
what is deposition like in the upper stage
- little deposition; mainly largest particles deposited in the river bed as energy levels drop
what is erosion like in the middle stage
- mainly lateral and by abrasion
- attrition of larger particles in this stage means that sediment particle size decreases from source to mouth
what is transportation like in the middle stage
- more material carried in suspension as particle size decreases
- some larger particles moved by saltation
what is deposition like in the middle stage
- sand and gravel are deposited across the flood plain as the river floods and friction reduces the rivers energy
what is erosion like in the lower stage
although velocity and discharge are highest, theres less erosion as turbulence is lower and sediment particle size is reduced
- some lateral erosion occurs during the formation of meanders
what is transportation like in the lower stage
- mainly smaller particles such as silt and clay carried by suspension or substances carried in solution
what is deposition like in the lower stage
- smaller particles such as sand silt and clay are deposited on the flood plain when the river floods and in the river mouth as the sea absorbs river energy
whats the cross profile like at upper/middle/lower stage
upper: steep v shapes, vertical erosion crates narrow valley floors and steeply sloped sides
middle: wider, caused by later erosion, deposition creates floodplain on the valley floor
lower: wide with gently sloping sides, much wider flood plain caused by deposition