Drainage Basin 3.1.1.2 Flashcards

1
Q

What is a drainage basin

A

Open, local hydrological cycle

Areas that is drained by a river and it’s tributaries

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2
Q

What’s the boundary of a drainage basin

A

The watershed as it separates basins

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3
Q

Inputs of a drainage basin

A

Rain, snow, hail

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4
Q

Outputs of a drainage basin

4

A

Evaporation, transpiration,evapotrainspiration, river discharge

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5
Q

6 stores

A

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

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6
Q

10 flows

A
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
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7
Q

What is a water balance
What does it affect
Formula

A

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

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8
Q

Rivers regime

A

Annual pattern of a river, with discharge levels rise and fall

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9
Q

6 parts of soil moisture graph and axis

A

Soil misfire recharge
Utilisation
Deficit
Surplus

Precipitation line
Potential evapotranspiration line

Precipitation
Month

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10
Q

What’s a hydrograph / flood hydro road

A

Graph to show discharge of a river

Flood - show discharge leading up to and after rainfall event

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11
Q

What’s river discharge

A

Volume of water that flows in a river per second measured in cubic meteres per second

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12
Q

8 parts of hydrographic

And axis

A
Lag time
River I flood
Peak discharge 
Peak rainfall
Base flow
Rising limb
Falling limb
Bankfull discharge 

Rain , time , discharge

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13
Q

Factors affecting hydrographic shale and run off

4 physical

A

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

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14
Q

Factors affecting hydrographic and run off

4 human

A

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

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