Drainage Basin 3.1.1.2 Flashcards
What is a drainage basin
Open, local hydrological cycle
Areas that is drained by a river and it’s tributaries
What’s the boundary of a drainage basin
The watershed as it separates basins
Inputs of a drainage basin
Rain, snow, hail
Outputs of a drainage basin
4
Evaporation, transpiration,evapotrainspiration, river discharge
6 stores
Interception - temporary, precipitation on vegetation canopy of buildings
Vegetation - water taken up and stored in plants
Surface - water in ponds, lakes etc
Soil- moisture in soil
Groundwater - water in ground. Porous rocks hold water - aquifers
Channel - water ina river or stream
10 flows
Infiltration Overland/run off Throughflow Stem flow Throughfall Percolation Groundwater flow Base flow - groundwater flow that feeds into river through river banks Inter flow - water flowing downhill through permeable rock Channel flow
What is a water balance
What does it affect
Formula
Balance between inputs and outputs
Affects how much water is stored in basin
P= Q+ E +- S
Q - discharge
E - evpotranspiration
S - changes in storage
Rivers regime
Annual pattern of a river, with discharge levels rise and fall
6 parts of soil moisture graph and axis
Soil misfire recharge
Utilisation
Deficit
Surplus
Precipitation line
Potential evapotranspiration line
Precipitation
Month
What’s a hydrograph / flood hydro road
Graph to show discharge of a river
Flood - show discharge leading up to and after rainfall event
What’s river discharge
Volume of water that flows in a river per second measured in cubic meteres per second
8 parts of hydrographic
And axis
Lag time River I flood Peak discharge Peak rainfall Base flow Rising limb Falling limb Bankfull discharge
Rain , time , discharge
Factors affecting hydrographic shale and run off
4 physical
Size of basin - larger catches more precipitation- higher peak discharge as larger distance to travel
Shape - circular = more flashy . All pints on watershed roughly same distance from point of discharge - more water reaches same point at same point
Steepness - water flows faster dounhill - shorten lag time
Rock and soil type - impermeable doesn’t store water - increases run off and peak discharge
Factors affecting hydrographic and run off
4 human
Deforestation - reduces interception and infiltration rate - rapid overland flow and flashy hydrograph. Also soil exposure - increased erosion - sedimentation of channel - reduces bankfull capacity - increased flood risk
Afforestation - oppose effect
Agriculture
Growth of urban areas - flashy due to impermeable surfaces