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Management Practices to Increase Nitrogen Retention and Decrease Losses in Agricultural Systems.
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Special Sessions
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Symposium--Management Practices Inpact on Soil Nitrogen Conservation
Monday, November 3, 2014: 1:00 PM
Long Beach Convention Center, Room 102A
David S. Powlson1, Keith W.T. Goulding2, Andrew J. Macdonald2, Paul R. Poulton1 and Chris van Kessel3, (1)Department of Sustainable Soils & Grassland Systems, Rothamsted Research, Harpenden, United Kingdom
(2)Rothamsted Research, Harpenden, United Kingdom
(3)University of California-Davis, Davis, CA
To achieve global food security greatly increased nitrogen (N) inputs to agriculture will be required, especially from fertilizers but also from more efficient recycling of N from manures and organic by-products and through inclusion of legumes in cropping systems. But increased inputs bring increased risks of N losses which cause environmental damage. Global estimates indicate that, on average, 50% of fertilizer N is unaccounted for in crop uptake or soil retention, implying a loss to the environment of about 50 Tg /yr. Timing, form and method of application of fertilizer N and slurries or manures can be adjusted to minimise direct losses, though it is common for decreased loss via one pathway to lead to an increase through another. A range of “precision farming” technologies can assist in improved targeting of N applications in timing, position or quantity. Various sensors are increasingly available, both tractor-mounted and linked to fertilizer delivery or hand-held chlorophyll meters suitable for small farmers. Even leaf color charts can be surprisingly beneficial for managing N timing by small-holder farmers in less developed regions. In some situations inhibitors of nitrification or urease activity are effective.
Predicting and managing N mineralized from soil organic matter, crop residues or manures is a central factor in improved N utilization, but in practice difficult to achieve. In temperate regions, 15N-fertilizer studies commonly show that some 20% of applied fertilizer N is retained in soil organic matter at the end of the first growing season; in tropical regions it is often double this. Residual organically-bound N is a source of N through future mineralization, but its release is slow. Intercropping cereals with legumes is useful in some systems. In the long-term inclusion of biological nitrogen fixing activity into cereal crops may be possible, but it is likely improved agronomy based on incremental understanding of N cycle processes and more precise management will be the key approach for many years.
See more from this Division:
Special Sessions
See more from this Session:
Symposium--Management Practices Inpact on Soil Nitrogen Conservation