A Canadian Agricultural Nitrogen Budget model was developed to calculate the agro-environmental indicators: Residual soil nitrogen (RSN) and Indicator of Risk of Water Contamination by Nitrogen (IROWC-N) for 3500 polygons of the 1:1 m Soil Landscapes of Canada scale. Residual Soil Nitrogen was calculated for the census years 1981, 1986, 1991, 1996 and 2001. These results were then used in conjunction with climate data to calculate over-winter N loss and its concentration in the drainage water. The main inputs were the acreages, yields and N recommendation rates for major crops, and the types and numbers of livestock. Various coefficients and assumptions were incorporated into the calculations. Validation of the model was carried out using provincial nitrogen sales data, and results showed good agreement between the calculated fertilizer N and the amount of fertilizer N sold in each province in 1996 and 2001. The two indicators were linked to outputs of the economic-based Canadian Regional Agricultural Model in order to assess the impacts of policy scenarios on nitrogen balance. At the national scale, the scenario of improved N fertilization practices reduced the RSN by 13%. RSN was also sensitive to the N2O:N2 ratio resulting from N losses through denitrification. Key words: Landscape nitrogen model, Agri-Environmental Indicator, Soil Landscapes of Canada, Census of Agriculture
K. 2007. Residual soil nitrogen indicator for agricultural land in Canada. Can. J. Soil Sci. 87: 167-177. Residual soil nitrogen (RSN) is the amount of inorganic nitrogen that remains in the soil at the end of the growing season after crops have been harvested. RSN is an estimate of this quantity, calculated as the difference between all N inputs (fertilizer, manure-N, biological fixation, and atmospheric deposition) and all N outputs (N removed in crop harvest, N lost from ammonia volatilization and N lost from denitrification) assuming that mineralization and immobilization are generally balanced. RSN was calculated on a soil polygon level (scale 1:1 million) as well as on provincial and national levels for each of the 5 census years from 1981 to 2001. The Canadian average RSN values from 1981 to 1996 were fairly constant with a range of 12.9 to 13.9 kg N ha -1 . However, RSN increased by 51% from 13.9 kg N ha -1 in 1996 to 21.0 kg N ha -1 in 2001. This dramatic increase was due to several factors including an increase in legume crop acreage (i.e., increased biological N 2 fixation) and lower crop yields and reduced N uptake as a result of climatic constraints (droughts) which were prevalent in many regions in Canada in 2001. On attribue cette hausse draconienne à plusieurs facteurs, y compris l'accroissement de la superficie consacrée à la culture des légumineuses (à savoir, augmentation de la fixation de N 2 par des processus biologiques), la diminution des rendements et une plus grande utilisation du N consécutivement aux contraintes climatiques (sécheresse), conditions qui prévalaient dans maintes régions du Canada en 2001.
Drriven by changes in agricultural production practices, nitrogen (N) inputs have increased steadily on Canadian farms. An agro-environmental indicator was developed to monitor potential water pollution by N: indicator risk of water contamination by nitrate-nitrogen (IROWC-N). The indicator links the residual soil nitrogen (RSN) indicator to climate and soil conditions to assess the likelihood of N moving through the soil and out of the agricultural system. The results are assessed in terms of Nlost via leached water (Nlost) and its concentration in the leached water (Nconc), with the IROWC-N risk classes based on Nlost and Nconc criteria. The estimated amount of Nlost in Canada ranged from 5.1 kg N ha-1 in 1991 to 6.4 kg N ha-1 in 2001. Nconc values remained fairly constant during the 1981 to 1996 census years (ranging from 3.7 to 4.5 mg N L-1), but increased sharply (27%) to 5.7 mg N L-1 in 2001 as compared with 1996. During the 1981 to 2001 period, close to 80% of the Canadian farmland area remained in the very low and low IROWC-N risk classes, but over the years 18% shifted to a higher risk class. In 2001, large areas (> 1 million ha) in the high risk IROWC-N class were found in Manitoba, southern and eastern Ontario and in Quebec. Provincial averages of Nlost over 5 census years (1981, 1986, 1991, 1996 and 2001) varied from less than 5 kg N ha-1 in Alberta and Saskatchewan to more than 20 kg N ha-1 in Ontario, Quebec and the Atlantic provinces. With the exception of Manitoba, provincial Nconc values did not exceed the Canadian drinking water guideline of 10 mg NO3-N L-1. In each of the census years, British Columbia, Alberta and Saskatchewan had more than 70% of the farmland area in the very low and low risk classes for IROWC-N. In Ontario and Quebec, most of the farmland area was either in the low or in the high risk class. More than 50% of the farmland area in New Brunswick, Nova Scotia and Newfoundland was in the very low, low and moderate risk classes, whereas in Manitoba and Prince Edward Island, more than 60% of the farmland was in the moderate and higher level risk classes for IROWC-N. Overall, the 20-yr trend in risk of water contamination by N was worsening. Key words: Water contamination by nitrogen, nitrate, water quality, Soil Landscapes of Canada, Census of Agriculture
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
hi@scite.ai
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.