Factors Affecting Transfer And Stores Of Matter In A Drainage Basin Flashcards
What are the 7 factors that affect stores and transfer of matter in a drainage basin
Urban areas
Seasons
Soil type
Rainfall
Geology
Relief
Nemonic for the 7 factors
USSR GR
Describe the affect of vegetation
THICK vegetation creates MORE opportunities for interception and evaporation from the leaves of trees
Any water that doesn’t reach the ground directly will take longer to go through the system
Describe the affect of soil type
POROUS (permeable) soils allow water to pass through and infiltrate quickly as the have big spaces within them SAND
NON POROUS (impermeable) soils do not allow water to infiltrate which means the rate of overland flow increases and the water reaches the river faster, increasing the chances of flooding CLAY
Describe the affect of seasons
WARMER temperatures of summer encourage MORE evapotranspiration which lowers the discharge levels in the river
HOT days reduces infiltration as the soil becomes hard baked
COLD days reduces infiltration as the soil becomes frozen
LEAVES FALLING in autumn reduces interception and more water reaches the ground directly, therefore reaching the river channel faster
Describe the affect of geology
POROUS (permeable) rock increases percolation and groundwater flow. This reduces the soil store and the amount of water transferred by overland flow, which means water takes a longer time to reach the river channel and the risk of flooding is reduced
Describe the affect of urban areas
LESS VEGETATION
LESS INTERCEPTION
LESS INFILTRATION
Due to the impermeable surfaces (tarmac)
Water travels directly to the via overland flow, drains and sewers
This increases the risk of flooding
Describe the affect of relief
STEEPER drainage basin means less opportunities for infiltration so surface runoff dominates
LOWLAND areas have more infiltration and water remains in the soil store for longer before being transferred via throughflow
Describe the affect of rainfall
HEAVY, INTENSE RAINFALL
rain may fall at a faster rate than the soil can accommodate infiltration
Soil may become saturated and waterlogged as infiltration capacity reached
Leading to the main transfer of overland flow