Lecture 2 - Sediment transport, Flashcards
Give three examples of mass wasting
Rock slide
Earth flow
Mud flow
What three factors increase mass wasting events
1) composition of material
2) Amount of h20 present
3) angle of the slope
What is meant by the angle of repose?
The angle in which the sediments will stack if dropped from a cosistant point above the center
What are the triggers for mass wasting?
1) earth quakes
2) heavy rain
3) gradual over steepening of slope
What effect did the building of the Vaiont Dam have with respect to the subsequent landslide
Effects magnified by the poor placement of the dam, killed 3000 people. Placement of the damn meant there was more pressure and the materials become more saturated. The ancient slide was ignored.
What is the difference between tublar and laminar flows
Laminar flows are parallel stream lines and simple flow. Turbalant flows are cross cuting stream lines and complex flows
What is suspended load
material suspended in the water istelf
What is the bed load
The material that is being dragged along the bottom, sliding and rolling
What is saltation?
Its the intermitant jumping of smaller rocks along the floor the river, grains are sucked up into eddies then moved further down and this repeats
Explain entrainment
Bernoulli’s Principle, The sum of verlocit and pressure on an object must be constant, this causes the low pressure of top of the rock to make it rise.
Define floodplain (river systems)
The area either side of the river which has been flooded before and may be again if flooding occours. Its a low land area.
Define: Channel (river systems)
The main flow of water through an area such as river
Dfine Levees (river systems)
When the river flood it deposites sediment either side of the river causing a slow build up of sediment on eithr side of the river bank
Define Terraces (river systems)
If the land is uplifted the river channel will erode downwards. The old flood plane will then form a terrace
Define: Alluvial Fan:
Fan shaped accumulations of sediment despoisted when a stream must suddelny adjust to a change in conditions, such as a mountain front