THE AMAZON RAINFOREST CASE STUDY
How do the water and carbon cycles operate in contrasting locations
FACTS ABOUT THE AMAZON:
Size: 7 million km2
Population: 30 million
Rivers: Purus, Maranon, Amazon - main river
Species: Over 3 million species
Vegetation: Over 40,000 species of trees/plants
WHY IS THE AMAZON IMPORTANT?
Plays a large part in the water cycle and temperature regulation
Exchanges oxygen with CO2 within the atmosphere
More than 1 trillion tonnes of CO2 per year are sequestered
WATER AND CARBON CYCLES IN THE TROPICAL RAINFOREST
High rates of evaporation - approx. 50% of rainfall is returned by evapotranspiration, mainly from leaf surface
Large stores of moisture in the atmosphere, realtive humidity is high
Rates of carbon fixation through photosynthesis are high
PHYSICAL FACTORS AFFECTING FLOWS AND STORES OF THE WATER CYCLE
Temperature
High temps = high rates of evapotranspiration
Covection leads to high humidity, storms and intese rainfall
Geology
Large areas of impermeable rock in the Amazon Basin - lead to high levels of run-off
Relief
Most of the Amazon Basin has gentle relief
Most water movement is by overland flow and throughflow
PHYSICAL FACTORS AFFECLING THE FLOWS OF THE CARBON CYCLE
Temperatures
High temperatures lead to rapid vegetation growth and large biomass of the Amazon - stores approx. 100 billion tonnes of carbon
Vegetation
60% of rainforest carbon is stored in the above-ground biomass trees
Organic matter in soils
leaf litter and dead organic matter accumulate at soil surface
Rapid decompositionand minerals are quickly taken up in the tree root systems
Mineral composition of rocks
Carbonates are largely absent from the mineral composition of igneous and metamorphic rocks of the Amazon Basin
IMPACTS ON FLOWS AND STORES IN THE DRAINAGE BASIN
Deforestation has led to flooding in some areas
Deforestation has led to reduced water storage in trees, soils and rocks
Fewer trees means less evapotranspiration and precipitation
Run-off increases
Impact of deforestation on the water cycle can change climate at local and regional scales, reduced humidity, cloud formation and precipitation, increased peak flows of riveres
IMPACT OF HUMAN ACTIVITY ON CARBON FLOWS, SOIL AND NUTRIENT STORES
Deforestation can exhaust the carbon biomass store
Deforestation can reduce the input of organic matter to the soil
Fewer decomposer organisms mean that the flow of carbon from the soil to the atmosphere is reduced
What nurtients remain are quickly eroded by run-off
STRATEGIES TO MANAGE THE TROPICAL RAINFOREST
Protection - e.g. Amazon Regional Protected Areas
Projects: reforestation projects e.g. Paraic project in Rohdônia
Improved argicultural techniques: diversification, rotational cropping and combining livestock and arable farming