Gross nitrogen mineralization in pulse-crop rotations on the Northern Great Plains
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- 作者：Angela Bedard-Haughn (1)
Louis-Pierre Comeau (1) (2)
Amy Sangster (1) (3) - 关键词：Isotope dilution ; Field pea ; Lentil ; Canola ; Wheat ; Chernozem
- 刊名：Nutrient Cycling in Agroecosystems
- 出版年：2013
- 出版时间：March 2013
- 年：2013
- 卷：95
- 期：2
- 页码：159-174
- 全文大小：284KB
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Louis-Pierre Comeau (1) (2)
Amy Sangster (1) (3)
1. Department of Soil Science, University of Saskatchewan, 51 Campus Drive, Saskatoon, SK, S7N 5A8, Canada
2. School of Biological Science, University of Aberdeen, 23 St. Machar Drive, Aberdeen, AB24 3UU, UK
3. Perennia, 199 Innovation Drive, Bible Hill, NS, B6L 2H5, Canada - ISSN：1573-0867
文摘
Pulse crops represent an ever-increasing proportion of cropping systems in the Northern Great Plains. Previous studies have noted apparent benefits associated with pulse crop production that extend beyond the reduced need for N fertilizer in the year of production; these benefits have been attributed to the quality of pulse residues and their effects on N dynamics in subsequent years. This study used isotope dilution techniques to quantify the N-cycling effects of pulse crops in the rotation. Gross N mineralization was measured over three growing seasons at two Agriculture and Agri-Food Canada research sites in Saskatchewan, Canada: Scott (four rotations; one with pulse crop) and Swift Current (three rotations; one with pulse crop). Gross nitrification and the relative contribution of nitrification vs. denitrification to N2O emissions were also measured. Across all dates and rotations, the average gross mineralization rate at Scott was 2.0?±?4.0?mg NH4 +-N?kg? soil d? and at Swift Current was 1.4?±?3.9?mg NH4 +-N?kg? soil d?. At both sites, rates were highly variable across the growing season, but tended to be higher at anthesis than either pre-seeding or post-harvest. The only significant difference among rotations was at Swift Current, where the fertilized continuous wheat rotation had the highest gross mineralization rates (rotation average: 2.3?mg NH4 +-N?kg? soil d?). The lack of difference among most rotations was particularly notable given the differences in residue quantity among the crops. Ultimately, the lower quantity of residues produced by pulse crops appears to be offset by their higher quality.