
In some years, however, we can be fairly certain that there was little nitrate in the soil profile at the end of the crop, and/or overwinter precipitation leached any residual to below the rootzone of the next corn crop. In order to save the work and expense of performing the PPNT when there is little likelihood of carryover, Larry Bundy and Mattias Vanotti of the Department of Soil Science, University of Wisconsin-Madison devised a calculation to identify years when the PPNT is not useful. The predictive relationship was based on the evaluation of long-term cropping trials at the University of Wisconsin-Madison College of Agricultural and Life Sciences Agricultural Research Station at Lancaster, WI. Descriptions of the calculation were published in:
Three factors were found to account for most of the year-to-year variation in nitrogen carryover:
August soil water and overwinter percolation was estimted using a computer simulation model of hydrology called GLEAMS (Version 1.8.55), developed by the USDA/ARS. Carry-over nitrogen was assessed both by soil analysis and the yield of oat crops which were grow on residual soil nitrogen.
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UNDER CONSTRUCTION |
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Creation of this Web-accessible version of the N carryover
calculator was funded by the
WISCONSIN FERTILIZER RESEARCH COUNCIL
For more information on nitrogen carryover research,
contact Larry G Bundy at the Dept. of Soil
Science, Univ. of Wisconsin-Extension
Larry Bundy, lgbundy@facstaff.wisc.edu