Soil carbon at Higher Level: The same ideas as SL, with different examples: soil carbon farming in Australia, Borneo's thin rainforest soils, the Congo's hidden peatlands, Kazakhstan's ploughed steppe and re-wetting bogs in northern England. At HL, link soil carbon to climate policy: who pays to keep it in the ground?
Practise this as you read
- Compare the two rates every time: input and decomposition.
- Quote chart values with units before you explain them.
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In versus out: Whether a soil is a carbon sink, a carbon store or a carbon source depends on two rates: how fast dead organic matter goes in, and how fast it decomposes.
The points to remember
- Carbon enters the soil as dead organic matter: leaves, roots, dung (plants took it from the air).
- It leaves as carbon dioxide, or methane where there is no oxygen, when decomposers break it down.
- Store: the amount of carbon the soil holds.
- Sink: dead matter added faster than it decomposes: the store grows and carbon is taken from the air.
- Source: decomposition faster than the input: the store shrinks and carbon is added to the air.
- Soils hold more carbon than the atmosphere and all plants put together.
Remember it as: More in than out: sink. More out than in: source.
Real example: in Australia, farmers can earn carbon credits from the government by proving that changes such as better grazing have raised the carbon stored in their soils.
Do not mix up store and sink: A store is an amount (tonnes of carbon). A sink is a process: carbon going in faster than it comes out. A soil can be a big store and still be a source if it is losing carbon.
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A tropical rainforest makes a huge amount of dead matter, so you might expect a thick, carbon-rich soil. In fact its soil holds little, because everything that falls is broken down and taken up again quickly.
The points to remember
- Warm and wet all year: decomposers work fast, so dead leaves are gone in months.
- Roots and fungi take the released nutrients back at once: most carbon stays in the trees, not the soil.
- Heavy rain leaches old, weathered soils, so little organic matter builds up.
- So the input is large, but decomposition keeps pace: the soil store stays small.
- In the chart: tropical forest about 120 t of carbon per hectare in plants, 123 t in the soil.
Remember it as: Hot and wet: carbon in the trees, not the soil.
Real example: in the lowland rainforests of Borneo, a fallen leaf can be gone in a few months, and the soil under the giant trees is thin and poor in organic matter.
Too cold or too wet to rot: Under tundra, in wetlands and in peat, dead matter builds up because decomposers can hardly work.
The points to remember
- Cold: decomposers work slowly; in permafrost the ground is frozen and decomposition almost stops.
- Waterlogged wetlands and bogs: no oxygen, so dead plants decompose very slowly and build up as peat.
- Input is small, but decomposition is slower still, so carbon builds up over thousands of years.
- Peatlands cover about 3% of the land yet hold about twice the carbon of all the world's forests.
- Permafrost soils hold about 1,500 billion tonnes of carbon, nearly twice the carbon in the atmosphere.
Remember it as: Cold or waterlogged: slow decay, big store.
Real example: in 2017, scientists mapped the Cuvette Centrale peatlands in the Congo Basin for the first time. They found peat up to about 6 m deep, holding about 30 billion tonnes of carbon.
Give the cause, then the effect on decomposition: Write 'the bog is waterlogged, so there is no oxygen, so decomposers work very slowly and peat builds up', not just 'it is wet'.
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Temperate grasslands have little carbon in their plants, but a great deal in their soils.
The points to remember
- Grasses put much of their growth below ground: deep, dense roots.
- Many roots die each year and new ones grow, a large, steady input of dead matter deep in the soil.
- Cold winters and dry summers slow the decomposers.
- Earthworms and burrowers mix organic matter downwards; fires leave charcoal, which hardly decays.
- Result: deep, dark, carbon-rich soils: about 236 t of carbon per hectare in the soil, only 7 t in plants.
Real example: in the 1950s the Soviet Union ploughed huge areas of steppe in Kazakhstan for wheat (the 'Virgin Lands'). Ploughing let air into the deep, carbon-rich soils, and much of their carbon was lost.
Grassland is not 'little carbon': Grassland plants hold little carbon, but its soils hold a lot. Read which bar the question asks about: plants or soil.
People can tip the balance: Anything that speeds up decomposition or cuts the input of dead matter can turn a soil from a sink into a source. Anything that does the opposite can turn it back.
The points to remember
- Draining peat lets air in: decomposition speeds up, so the soil becomes a source; dry peat can also burn.
- Ploughing breaks the soil open to air, so stored carbon is decomposed and lost.
- Clearing forest cuts the input of dead matter and leaves soil open to erosion.
- Warming speeds up decomposers and thaws permafrost, releasing carbon dioxide and methane.
- Back to a sink: no-till farming, cover crops, compost, re-wetting peat, planting trees.
Sink to source
- Drain peat
- Plough grassland
- Clear and burn forest
- Warm and thaw permafrost
Source to sink
- Re-wet peat
- No-till and cover crops
- Add compost or manure
- Plant trees, restore grassland
Real example: the Great North Bog project in northern England is blocking old drainage ditches to re-wet peat moors, so they stop losing carbon and start storing it again.
Name the rate that changes: Say whether an action changes the INPUT of dead matter or the rate of DECOMPOSITION, and which way.
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How this comes up: Paper 1 or Paper 2, Section A: use a chart to explain a difference in soil carbon [3]. Quote the values, then explain with input and decomposition.
The figure shows the carbon stored in plants and in the soil in six biomes.
With reference to the figure, explain why temperate grassland soils store more carbon than tropical forest soils.
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