Underestimation of carbon dioxide emissions from organic-rich agricultural soils

Abstract

Organic-rich agricultural soils, including drained peatlands, are hotspots for biogenic CO₂ emissions. Due to microbial mineralisation, the organic carbon (OC) content of these soils transitions to that of mineral soils, but it remains unclear how the residual OC content controls the rate of CO₂ emission. Here we show that area-scaled CO₂ emissions from topsoils with >6% OC are not controlled by OC content and OC density in a comprehensive laboratory incubation experiment. National greenhouse gas inventories assign area-scaled CO₂ emission factors to soils with >12% OC, while soils with 6-12% OC are mostly disregarded or treated with lower emission factors. In this respect, our results suggest that CO₂ emissions from organic soils could be underestimated by up to 40% in the Danish national inventory submission to the United Nations Framework Convention on Climate Change (UNFCCC). We conclude that global underestimation of area-scaled CO₂ emissions from 6-12% OC soils occurs in countries with large proportions of organic soils in transition from organic to organo-mineral soils due to agricultural management. Refining CO₂ emission estimates for 6-12% OC soils is critical for the accuracy of national inventories, but also for recognising the climate benefits of initiatives to rewet drained organic soils.

Emissions of CO2 from drained peat soils with 6- 12% organic C can be as high as those from soils with >12% organic C. This was shown in an incubation study of >100 organic soils, and may have implications for national greenhouse gas inventories.