CCEA A-Level Geography 3910
Processes That Shape Fluvial Environments
Human Interaction in Fluvial Environments
Global Biomes
Small-Scale Ecosystems
The Processes That Shape Our Weather and Climate
Weather in the British Isles
Global Weather Issues
Population Data
Population Change
Population and Resources
Settlement Change and the Rural-Urban Fringe
Planning in Rural Environments
Urban Challenges in MEDC and LEDC Cities
Measuring Development
Reducing the Development Gap
Emerging Markets
Data Collection
Data Processing
Fieldwork Skills and Techniques
Planning and Recording an Investigation
Plate Tectonics: Theory, Margins and LandformsTectonics
Volcanic Activity and Its ManagementTectonics
Seismic Activity and Its ManagementTectonics
Locations and Climates of the Major Tropical BiomesTropical
Management and Sustainability in Arid and Semi-Arid Tropical EcosystemsTropical
Management and Sustainability in the Tropical Forest EnvironmentTropical
Coastal Processes and FeaturesCoastal
Regional Coastlines: Submergence, Emergence and Rising Sea LevelCoastal
Coastal Management and SustainabilityCoastal
Natural Climate Change: Evidence, Causes and the Arrival of the HoloceneClimate
Lowland Glacial LandscapesClimate
Current Global Climate Change: Human Causes and ImpactsClimate
Managing Global Climate ChangeClimate
Cultural Groups, Social Inequality and LandscapeCultural
MigrationCultural
The Geographies of CyberspaceCultural
Sustainable Development in SettlementsPlanning
Urban Design, Planning and Management for SustainabilityPlanning
Traffic and TransportPlanning
Defining EthnicityEthnic
Processes That Create and Maintain Ethnic DiversityEthnic
Ethnic ConflictEthnic
The Changing Nature of TourismTourism
Challenges and Management of Mass TourismTourism
Ecotourism: Opportunities, Challenges and RegulationTourism
Decision Making in Geography
Human Interaction in Fluvial Environments
Environmentally sensitive and sustainable river management
- 3 things to know
- Unit AS 1
Overview
Sustainable river management, advantages and disadvantages of washlands and limitations of afforestation as a flood management strategy.
What you need to know
Answer each one before you reveal it.
How does afforestation in the upper catchment reduce flood risk?
What is land-use zoning on a floodplain?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is meant by sustainable river management?
Model answer
Managing the river so that flood risk is reduced in a way that can be maintained indefinitely without excessive cost, without damaging the river ecosystem and without passing the problem on to other places or to future generations. It works with natural processes rather than against them - storing and slowing water rather than only speeding its removal - and it accepts that some flooding of the floodplain is natural and should be accommodated in the right places rather than prevented everywhere.
- 2
What is a washland?
Model answer
A washland is an area of the floodplain that is deliberately set aside to be flooded when the river exceeds a certain discharge. It is kept free of housing and permanent structures and is used instead for rough grazing, hay meadow, playing fields, wetland nature reserve or informal recreation, so that when it floods the damage is negligible. Water may be allowed to spill onto it naturally over a lowered bank or be admitted through a controlled sluice.
- 3
How does a washland reduce flooding downstream?
Model answer
It provides temporary storage that takes water out of the channel exactly when discharge is at its highest. Diverting part of the flood peak into the washland lowers the volume passing downstream at that moment, so the downstream peak discharge is reduced and, because the stored water is released slowly afterwards, it is also delayed and spread over a longer period. On a storm hydrograph the effect is to flatten and broaden the peak. Several washlands along a catchment can attenuate a flood wave substantially.
- 4
What are the advantages and disadvantages of washlands?
Model answer
The advantages are that they are cheap to create and to maintain compared with engineered defences, they store rather than transfer the water so downstream communities benefit too, they create valuable wetland habitat for wading birds and aquatic species, the deposited silt maintains soil fertility, and they can provide public open space. The disadvantages are that they need a large area of floodplain, which may not exist in a built-up catchment, that land is taken out of intensive agricultural or development use and owners must be compensated, that farming on them is restricted to low-value uses and timing is uncertain, and that in a very large event the storage fills and can offer no further protection.
- 5
How does afforestation in the upper catchment reduce flood risk?
Model answer
Trees intervene at several points in the drainage basin system. The canopy intercepts rainfall so that some of it evaporates without ever reaching the ground, and the rest is delayed as it reaches the soil by throughfall and stemflow. Transpiration continuously draws water out of the soil, keeping soil moisture storage available to absorb the next storm. Roots create channels that raise infiltration capacity, so water enters the soil and travels slowly as throughflow instead of rapidly as overland flow, and the litter layer physically obstructs any surface flow. Roots also bind the soil, reducing erosion and so limiting the sediment that would otherwise silt up the channel downstream. The overall effect is a longer lag time and a lower peak discharge.
- 6
What are the limitations of afforestation as a flood management strategy?
Model answer
It takes decades to become fully effective, since young trees intercept and transpire very little, so it does nothing about the risk facing a community today. It requires large areas of upland to be taken out of farming, which affects rural livelihoods and requires compensation or subsidy. Dense conifer plantations can acidify soils and streams, support little biodiversity and look uniform, and the ploughing and drainage used to establish them can actually increase runoff in the early years, as can clear-felling later. Most importantly, its effect is greatest on small and moderate storms; in a prolonged, extreme event the soil beneath the trees becomes saturated too, and the reduction in peak discharge is much smaller.
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