Thursday, 13 July 2006
70-4

Nitrogen Management Under Maize in Humid Regions: The Case for the Dynamic Approach.

Harold M. Van Es1, Beverly Kay2, Jean Sogbedji2, Jeffrey Melkonian2, R.S. Dharmakeerthi2, Hunaira Dadfar2, and Ivy Tan2. (1) Cornell University, 1005 Bradfield Hall, Ithaca, NY 14853, (2) University of Guelph, Stone Rd E, Guelph, ON N1G 2W1, Canada

Nitrogen is an essential crop nutrient that has been a focus of soils research for almost two hundred years. In humid regions, N transformations are strongly influenced by dynamic processes that may result in rapid losses, mostly through leaching and denitrification. These losses of N result from complex interactions among weather, soil hydrology, crop water and N uptake, and management practices. Most current recommendations for N management do not directly account for the dynamic behavior of soil N, limiting our ability to more precisely and efficiently manage N. Increasing N fertilizer cost, elevated concerns about water contamination, and increased evidence of greenhouse gas impacts are prompting a new look at N management. This presentation will summarize results of experiments that demonstrate the need for a dynamic approach to N management under maize, and the importance of precise rates and timing. It recognizes that real-time weather significantly influences crop N availability on the short term. We will examine five maize N response studies conducted in New York, USA and Ontario, Canada for multiple years at multiple locations. All studies involve a spatial and a temporal component in that different soil types and landscape positions were involved and the studies were conducted for multiple years. Results show that crop N availability varies greatly from year to year based on weather conditions. High precipitation during the critical late spring period, when maize ET is still low and soil nitrate levels and temperatures have increased, is a strong determinant for N losses through leaching and denitrification, and thereby greatly affects crop N availability. This process may in some cases interact with soil type and landscape position, where finer-textured, poorly-drained soils, or lower-landscape-position soils may experience greater losses. This is the result of higher denitrification losses despite generally higher N supply capacity. Accurately predicting fertilizer-N requirements therefore requires a dynamic approach that incorporates this complexity. Soil N tests are expensive, primarily due to high labor costs, and high spatial and temporal variability makes their prediction accuracy often unsatisfactory. Computer simulation-based approaches are showing considerable promise for accurately predicting this seasonal variation in N dynamics and may be used to improve the environmental and economic aspects of N fertilization. Due to the critical nature of weather, soil and crop variables, such models need to accurately represent the important processes and be dynamically linked to real-time weather information. Similarly, in-field spectral sensing may provide such opportunities, although, like late-spring nitrate tests, it has the drawback of single-time assessment. In summary, increased N use efficiency and lower leaching and denitrification (incl. N2O) losses cannot be materialized in humid regions with static and spatially-uniform recommendations, and effective methodologies need to be developed for a more sophisticated and dynamic approach.

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