The drainage basin system Flashcards
Drainage Basin
An area of land drained by a rive and its tributaries
* Edge of basin is marked by boundary called watershed
* Vary in size e.g Missipssipi, Nile and Amazon
* Its an open system
Stores and Transfers
- Water enters basin as precipitation, some intercepted by vegetation, some drips as stemflow
- Groundwater flow feeds river banks and beds, slow transfer
- Infiltration occurs also. Infiltration capacity refers to what extent the soil is already saturated and is exceeded when soil is unable to absorb the water
- Overland flow where water runs off the surface
- Throughflow can occur where water is soil water until it reaches the water table
Water Balance
- Helps hydrologists to plan for future water supply and flood control
- P = Q + E +/- S (precipitaion, total runoff, evapotranspiration, storage)
Total runoff
A measure of the proporton of the total precipitation that makes its way into rivers and streams
* Varies with differences in soil water, rock type and vegetation cover
* Intensity of precipitation is also important
Discharge
Volume of water passing through a certain point in a river
* Measured in cumecs
* Discharge (m^3 per second) = cross sectional area (m^2) x velocity
Flood hydrograph
A graph showing the discharge of a river after a storm event
* It has 6 main features: falling + rising limb, peak discharge, peak rainfall, lag time and baseflow
Lag time
Time taken between peak rainfall and peak discharge
Rising + falling Limb
- Rising limb- when the river discharge rises
- Falling limb- where the river dicharge falls
Baseflow
Flashy hydrograph
Respond quickly to storm event
* Short lag time and high peak rainfall
* Small basins
* Impermeable rocks lead to overland flow
* Urbanisation encourages rapid water transfer
* Steep slopes lead to rapid water transfer
* Saturated soils leads to rapid overland flow
* Heavy rain exceeds infiltration capacity
Subdued hydrograph
Responds more slowly with an attenuated hydrograph
* Large basins mean slow water transfer
* Permeable rocks encourage slow transfer
* Forests/interception slow down water transfer
* Gentle slopes slow down water transfer
* Dry soils soak up water and slows down its transfer
* Light rain