Philippe Rochette1, Devon Worth2, Reynald Lemke2, Brian McConkey3, Raymond Desjardins4, Edward Huffman2, Dan Pennock5, Anthony Brierley2, Jingyi Yang2, Samuel Gameda2, and Julian Hutchinson2. (1) Agriculture & Agri-Food Canada, 2560 Hochelaga Boulevard, Ste-Foy, QC G1V 2J3, Canada, (2) Agriculture and Agri-Food Canada, Carling Avenue, Ottawa, ON K1A 0C6, Canada, (3) Agriculture Canada, Box 1030, Swift Current, SK S9H 3X2, Canada, (4) Agriculture Canada Research Branch, 960 Carling Neatby Building, Ottawa, ON K1A 0C6, Canada, (5) University of Saskatchewan, 51 Campus Drive, Saskatoon, SK S7N 5A8, Canada
International initiatives such as
the United Nations Framework Convention on Climate Change and the Kyoto
Protocol require that countries calculate national inventolries of their
greenhouse gas emissions. The objective of the present study was to develop and
use a Tier II methodology for the inventory of N2O emissions from
agricultural soils in Canada. Regional fertilizer-induced emission factors
(FIEF) were first determined using available field experimental data. Values for FIEF ranged from 0.0016 kg N2O-N kg-1 N
in the arid brown soil zone of the Prairies to 0.012 kg N2O-N kg-1 N in the humid eastern
provinces. A function relating FIEFs to climate (P/PE; P: precipitations PE:
potential evapotranspiration) was developed and used to estimate annual emissions
at the ecodistric level (avg. area: 430, 000 ha). Algorithms were also developed to account for
the effect of soil texture, spring thaw, topography, no-till, summerfallow and
irrigation on N2O emissions. Total direct N2O emissions
from agricultural soils averaged 36.8 Gg N yr-1 between 1990 and
2004 with variations from 32.4 (2001) to 45.2 Gg N yr-1 (2004). These estimates are approximately 40% lower
than estimates obtained using the IPCC Tier I methodology. Differences in N2O estimates
between the two approaches mainly arise from the use of lower emission factors
in the Tier II than in the Tier I methodology. Application of mineral N
fertilizers was the most important single source of soil N2O with
average emissions during the 1990-2004 period of 13.5 Gg N yr-1 or
36% of direct emissions. Crop residues
(9.0 Gg N yr-1; 24%), grazing animals (7.6 Gg N yr-1;
20%) and manure applied to soils (4.6 Gg N yr-1; 12%) were the other
major soil N2O sources.