factors affecting stream energy & channel processes Flashcards
3 main factors
- Resistance of bed material
- Load calibre
- Type of flow
Resistance of material
More resistant rock type = mone energy needed for water to flow
- more collusive material (i.e. finer material) = fewer changes in channel morphology
Factors affecting:
- vegetation
- degree of particle consolidation& cementation
- particle size
Load calibre
Size of individual particles carried by a river
- larger calibre seen in the upper course⇒ coarser sediments get deposited first upstream
Flow type
More turbulent flow = mone energy required/used
- helicoidal flow ⇒ corkscrew motion (more turbulent)
- laminar flow ⇒ no mixing between layers of water
3 channel processes
- Deposition
- Transportation
- Erosion
4 erosional processes
- Hydraulic action → high velocity water dislodges particles/fragments of unconsolidated material
- abrasion → mechanical breakage of sediment load by particles grinding against one another
- corrosion → when chemical reactions take place with rock surfaces
- attrition → breakdown of sediment load
directions of erosion
- vertical → downward cutting of the channel bed at the upper course
- lateral → erosion of the channel banks, where there is side-cutting because of high discharge levels
- headward → backwards erosion along the long profile, when adjusting to changes in stream energy
deposition
when stream energy falls → river cannot carry existing sediments & maintain discharge levels → larger sediments get deposited [first]
- happens because of flow deceleration or precipitation events that cause the load calibre to increase
3 transport processes
- traction → transport of large particles via sliding & rolling on the channel bed
- saltation → traction & suspension [particles get uplifted by turbulent forces & can set other particles in motion]
- suspension → transport of FINE particles as suspended load