1.6.2

Processes in a Drainage Basin

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Processes in a Drainage Basin

Key hydrological processes in rivers and drainage basins include precipitation, interception, infiltration, percolation, throughflow, groundwater flow, transpiration, evaporation, and evapotranspiration.

Precipitation and interception

Precipitation and interception

  • Precipitation delivers water to drainage basins as rain, snow, sleet, or hail.
  • Interception occurs when vegetation or surfaces catch precipitation, delaying its reach to soil.
Infiltration and percolation

Infiltration and percolation

  • Infiltration is the process of water entering the soil from the surface.
  • Percolation follows infiltration as water moves deeper through soil layers into rock.
Throughflow and groundwater flow

Throughflow and groundwater flow

  • Throughflow moves water laterally through soil towards river channels.
  • Groundwater flow involves the slow movement of water in rock layers beneath the soil.
Evaporation and Transpiration

Evaporation and Transpiration

  • Evaporation is when water from surfaces move back into the atmosphere.
  • Transpiration is the process where plants release water vapor into the air from their leaves.
Evapotranspiration

Evapotranspiration

  • Evapotranspiration combines evaporation and transpiration to move water back into the atmosphere.
Overland flow and channel flow

Overland flow and channel flow

  • Overland flow is water that moves over the land surface after heavy rain.
  • Channel flow is water moving in rivers and streams within defined channels.
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Paper 1 - Climate Change

6

Paper 2 - Changing Populations

7

Paper 2 - Changing Towns & Cities

8

Paper 2 - Development

9

Paper 2 - Changing Economies

10

Paper 2 - Resource Provision

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