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Nitrous oxide emission factors for agricultural soils in Great Britain: the impact of soil water‐filled pore space and other controlling variables
Author(s) -
Dobbie Karen E.,
Smith Keith A.
Publication year - 2003
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 - 10.1046/j.1365-2486.2003.00563.x
Subject(s) - arable land , grassland , soil water , environmental science , nitrous oxide , growing season , agronomy , nitrogen , agriculture , characterisation of pore space in soil , hydrology (agriculture) , soil science , ecology , chemistry , biology , geology , porosity , geotechnical engineering , organic chemistry
Measurements were made of nitrous oxide (N 2 O) emissions from N‐fertilised ungrazed grassland and arable land at sites widely distributed across Great Britain during 1999–2001. The closed static chamber method was used throughout. Emissions varied widely throughout the year at each site, and between sites. Daily fluxes up to 1200 g N 2 O–N ha − 1 d − 1 were recorded. The highest annual flux was 27.6 kg N 2 O–N ha − 1 at a grassland site in Wales, whereas the lowest, 1.7 kg N 2 O–N ha − 1 , occurred on a soil overlying chalk in southern England. The key factors affecting N 2 O emissions from agricultural soil were soil WFPS, temperature and soil NO 3 – –N content. On grassland, rainfall (particularly around the time of N application), with its consequent effect on water‐filled pore space (WFPS), was the main driving factor during the growing season. Annual emission factors (EFs), uncorrected for background emission, varied from 0.4 to 6.5% of the nitrogen (N) applied, covering a similar range for grassland to that found previously for sites restricted to Scotland. Continued monitoring at a grassland reference site near Edinburgh showed that annual EFs vary greatly from year to year, even with similar management, and that several years' data are required to produce a robust mean EF. The overall distribution of EFs in this and previous studies was log‐normal. The EFs for small‐grain cereals (and oilseed rape) peaked at a much lower value than those for grassland, whereas the values for leafy vegetables and potato crops fitted well into the grassland distribution. These differences in EF between various types of crop should be taken into account when compiling regional or national N 2 O emission inventories.