Abstract
Abstract. The application of nitrogenous fertilisers to agricultural soils is a major source of anthropogenic N2O emissions. Reducing the nitrogen (N) footprint of agriculture is a global challenge that depends, among other things, on our ability to quantify the N2O emission intensity of the world's most widespread and productive agricultural systems. In this context, biogeochemistry (BGC) models are widely used to estimate soil N2O emissions in agroecosystems. The choice of spatial scale is crucial because larger-scale studies are limited by low input data precision, while smaller-scale studies lack wider relevance. The robustness of large-scale model predictions depends on preliminary and data-demanding model calibration/validation, while relevant studies often omit the performance of output uncertainty analysis and underreport model outputs that would allow a critical assessment of results. This study takes a novel approach to these aspects. The study focuses on arable eastern Scotland – a data-rich region typical of northwest Europe in terms of edaphoclimatic conditions, cropping patterns and productivity levels. We used a calibrated and locally validated BGC model to simulate direct soil N2O emissions along with NO3 leaching and crop N uptake in fields of barley, wheat and oilseed rape. We found that 0.59 % (±0.36) of the applied N is emitted as N2O while 37 % (±6) is taken up by crops and 14 % (±7) is leached as NO3. We show that crop type is a key determinant of N2O emission factors (EFs) with cereals having a low (mean EF<0.6 %), and oilseed rape a high (mean EF=2.48 %), N2O emission intensity. Fertiliser addition was the most important N2O emissions driver suggesting that appropriate actions can reduce crop N2O intensity. Finally, we estimated a 74 % relative uncertainty around N2O predictions attributable to soil data variability. However, we argue that higher-resolution soil data alone might not suffice to reduce this uncertainty.
Highlights
The emission of N2O from agricultural soils is a interesting aspect of the global N cycle because it represents a key contribution of modern agriculture to climate change which, in turn, poses a serious threat to agriculture itself (Paustian et al, 2016)
It shows (1) that the soil N2O emission factors (EFs) for cereals is well below the generic Intergovernmental Panel on Climate Change (IPCC) EF of 1 %; (2) that winter oilseed rape cultivation contributes to much higher N2O emissions than that of cereals; and (3) that the soil N2O emissions are the result of dynamic interactions between different factors, of which only fertiliser N was identified as having a clear effect on all simulated variables
We conclude that, while the N footprint of northwestern European croplands is affected by inherent edaphoclimatic conditions, human decisions on cropping patterns and fertilisation largely control direct soil N2O emissions
Summary
The emission of N2O from agricultural soils is a interesting aspect of the global N cycle because it represents a key contribution of modern agriculture to climate change which, in turn, poses a serious threat to agriculture itself (Paustian et al, 2016). The emission of N2O from agricultural soils is controlled by the microbe-mediated processes of nitrification and denitrification These processes are tightly coupled and are affected by the combination of environmental conditions; the soil’s physical and biochemical composition; and the amount, timing and type of the applied fertiliser (Smith, 2017). These facts suggest that soil N2O emissions are highly variable both spatially and temporally, which makes measuring and predicting soil N2O difficult (Cowan et al, 2014). The Intergovernmental Panel on Climate Change (IPCC) stated
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