Unit 6: Changing carbon stores in peatlands over time Flashcards
What is peat?
Peat is a soil which over 80% is composed of partially decomposed organic matter, which has accumulated under certain condititions.
What are the conditions which peat requires to accumulate?
- climate where precipitation exceeds evaporation
- waterlogged ground (impermeable rock, high water-table, drainage depressions in landscape)
- oxygen deficiency (anaerobic conditions)
Where is high amounts of peat found?
The northern hemisphere. Links to geology as there is a lot of impermeable rock so the water cannot percolate downwards so it keeps the soil saturated.
Describe peat coverage in the UK?
In the UK peatlands cover around 3 million hectares or 12% of the land area and store over 3.2 billion tonnes of carbon.
What are the 3 main types of peatland in the UK?
Fen peatlands = in areas of low lying topography where groundwater meets the surface.
Blanket peatlands = occur on flat hill tops, with impermeable rocks where drainage is impeded.
Raised bogs = occur in topographical depressions/valley bottoms where drainage of water from the surrounding landscape accumulates.
Whats an example of a Fen peatland?
East Anglian Fens
Whats an example of a Blanket peatland?
The ‘Flow Country’ Sutherland, Scotland
Whats an example of raised bog?
Whixall Moss, Shropshire/Welsh Border
(main case study)
Describe peat in the carbon cycle?
Peatlands occupy 3% of the global land surface and are one of the earths major carbon sinks storing 500 gigatons of carbon. They are vitally important in the global carbon cycle.
How does peat form?
Peat forms in waterlogged areas, lacking in oxygen and where the water is acidic. In these conditions’ decomposition is restricted so that dead organic matter doesn’t decompose. Over thousands of years peat accumulates at the rate of 1mm per year. Consequently, carbon is preserved and makes up 50% of the DOM.
What happened with peat during the End of Devensian Glaciation (12000ybp)?
Kettle hole lake/depressions left by retreating glacier fills with water. Vegetation around the edges of the lake die and fall in.
What happened with peat during Holocene (last 10000 years)?
Lakes became inhospitable for many plants and water species - decomposition is inhibited.
Whats happening with peat in Present Day?
New types of plants such as sphagnum mosses, colonized the surface of the fen and as they dies and accumulated, transformed the fen into a swap bog. 80% is dead organic matter and of that 50% is carbon.
Why is sphagnum Moss a key species in peat formation?
It can hold around 20 times its own weight in water, effectively acting as a sponge and helps maintain waterlogged conditions.
As it grows it takes up nutrients such as potassium and magnesium from the environment and releases hydrogen ions; hence making the water acidic typically below pH 4.5.
It releases a chemical called sphagnum which has antibacterial properties and reduces decay of organic matter.
What are some human activity’s which threaten the peat bogs and impact on carbon and water cycles?
- Cutting Peat and burning it as a fuel (releases CO2)
- Cutting Peat and use in horticulture (gardening which has increased demand)
- Drainage of peat and use for agriculture or forestry