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Projecting future N 2 O emissions from agricultural soils in Belgium
Author(s) -
ROELANDT CAROLINE,
DENDONCKER NICOLAS,
ROUNSEVELL MARK,
PERRIN DOMINIQUE,
VAN WESEMAEL BAS
Publication year - 2007
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2006.01273.x
Subject(s) - environmental science , climate change , longitude , latitude , soil water , agriculture , greenhouse gas , agricultural land , land use, land use change and forestry , land use , climate model , climatology , atmospheric sciences , geography , soil science , ecology , geodesy , archaeology , geology , biology
This study analyses the spatial and temporal variability of N 2 O emissions from the agricultural soils of Belgium. Annual N 2 O emission rates are estimated with two statistical models, MCROPS and MGRASS, which take account of the impact of changes in land use, climate, and nitrogen‐fertilization rate. The models are used to simulate the temporal trend of N 2 O emissions between 1990 and 2050 for a 10′ latitude and longitude grid. The results are also aggregated to the regional and national scale to facilitate comparison with other studies and national inventories. Changes in climate and land use are derived from the quantitative scenarios developed by the ATEAM project based on the Intergovernmental Panel on Climate Change‐Special Report on Emissions Scenarios (IPCC‐SRES) storylines. The average N 2 O flux for Belgium was estimated to be 8.6 × 10 6 kg N 2 O‐N yr −1 (STD = 2.1 × 10 6 kg N 2 O‐N yr −1 ) for the period 1990–2000. Fluxes estimated for a single year (1996) give a reasonable agreement with published results at the national and regional scales for the same year. The scenario‐based simulations of future N 2 O emissions show the strong influence of land‐use change. The scenarios A1FI, B1 and B2 produce similar results between 2001 and 2050 with a national emission rate in 2050 of 11.9 × 10 6 kg N 2 O‐N yr −1 . The A2 scenario, however, is very sensitive to the reduction in agricultural land areas (−14% compared with the 1990 baseline), which results in a reduced emission rate in 2050 of 8.3 × 10 6 kg N 2 O‐N yr −1 . Neither the climatic change scenarios nor the reduction in nitrogen fertilization rate could explain these results leading to the conclusion that N 2 O emissions from Belgian agricultural soils will be more markedly affected by changes in agricultural land areas.