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How much carbon do soils store? A lot. At about 2.4 trillion tonnes of carbon, soil is the largest terrestrial carbon pool, and the top 2 metres of the planet’s soils hold four times as much carbon as all the world’s plants. Carbon stored in soil can also stay there for a very long time relative to carbon in plants
How much carbon do soils store? A lot. At about 2.4 trillion tonnes of carbon, soil is the largest terrestrial carbon pool, and the top 2 metres of the planet’s soils hold four times as much carbon as all the world’s plants. Carbon stored in soil can also stay there for a very long time relative to carbon in plants
A new bid to boost the amount of carbon stored in the world's soils has been launched at the Paris climate summit
Budiman Minasny, Alex McBratney &
Brendan Malone/ The Conversation
The world’s soils could be a key ally in the fight to limit global warming to 2℃, thanks to their ability to store carbon and keep greenhouse gases out of the atmosphere.
France’s Agriculture Minister Stéphane Le Foll has founded an ambitious international research programme, called “4 pour mille” (“4 per 1000”), which aims to boost the amount of carbon-containing organic matter in the world’s soils by 0.4% each year. The programme was launched officially at the United Nations climate summit in Paris, with the hope to sign up as many nations as possible.
How much carbon do soils store? A lot. At about 2.4 trillion tonnes of carbon, soil is the largest terrestrial carbon pool, and the top 2 metres of the planet’s soils hold four times as much carbon as all the world’s plants. Carbon stored in soil can also stay there for a very long time relative to carbon in plants.
Thanks to recently published maps of global soil carbon stocks, we can work out how much extra carbon needs to be stored in soils (and where) in order to meet the target.
The size of the task
There are roughly 149 million square kilometres of land in the world, so if all the world’s soil carbon were dispersed evenly there would be 161 tonnes per hectare. Hitting the 0.4% target would mean increasing soil carbon stocks by 0.6 tonnes (600 kg) of carbon per hectare per year, on average.
But of course, soils around the world vary widely in carbon storage – tropical peat soils, for example, hold about 4,000 tonnes of carbon per hectare, whereas sandy soils in arid regions may only hold 80 tonnes per hectare. The type of above-ground vegetation and how quickly the soil microbes use the carbon can also affect the amount of storage. Generally speaking, only a quarter of organic matter added to soil ends up being stored as carbon in the long term.
Farmers and other landowners would need detailed information about what exactly they will need to do to their own soils to boost their stored carbon by the required amount.
Is the target achievable?
Studies around the world suggest that soil carbon can potentially be stored at a rate of 500 kg of carbon per hectare per year – slightly below the average target – by reducing tillage and planting legume cover crops.
These estimates change with soil type and climatic regions. Our research suggests that some cropland areas of the world have the potential to hit the 0.4% target, locally at least, through more modest overall increases in carbon storage. Restoring the soil’s carbon content in these areas is a win-win situation, as it will offset greenhouse gas emissions and boost soil quality at the same time.
One such place is Australia, where current soil carbon estimates suggest that the 0.4% target could be met by boosting soil carbon by just 220 kg per hectare – something that could easily be delivered in places that are not suffering drought.
The “4 per 1000” aspiration is an ambitious one, but perhaps even more important is the effect this initiative will have on promoting good soil management, which in turn can help to mitigate climate change. By encouraging farming practices that store more carbon, we can also help farmers improve the quality of their soils and boost food security at the same time.
(Courtesy: http://scroll.in; Authors are: Budiman Minasny, Associate Professor in Soil Modelling, University of Sydney; Alex McBratney, Professor of Soil Science, University of Sydney; Brendan Malone, Research fellow, University of Sydney; and Uta Stockmann, , University of Sydney. This article was originally published on The Conversation)
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