Prepared by: G.K. Evanylo, Extension Soil Scientist, Waste Management & Water Quality, Virginia Tech; M. M. Alley, Extension Agronomist, Soil Fertility & Cropping Systems, Virginia Tech
Publication Number 418-016, Posted July 1998
Nitrogen and Corn Production
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Nitrogen Soil Test Procedure
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Nitrogen Behavior and Soil Testing
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Nitrogen Recommendations
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Pre-sided Soil Nitrate Test
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References
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Nitrogen use efficiency is the percentage of applied N that is actually taken up by the crop. Nitrogen use efficiency is normally 50-60%, but can be as high as 75% with proper N timing and placement. Costs of N fertilizers and environmental concerns about nitrate (NO3) from fertilizers, manures, and other nutrient sources leaching into groundwater require that new tools be developed and implemented to improve the use of all N sources available to the corn crop.
Many sources of N can be used by a corn crop. Residual N is N that is carried over in the soil from one growing season to the next, and this N source may supply as little as 10% or as much as 100% of the crop's total N need. Residual N is generally low under our climatic conditions because it tends to leach out of the root zone as NO3-N during the winter and early spring months; however, residual N can meet a significant portion of a subsequent corn cropıs need in silty and clayey soils, which retain more N than sandy soils. Most residual N is found in organic forms such as animal manures, legume forage and cover crops, and biosolids (municipal wastewater treatment sewage sludge).
The N that is in the organic forms becomes available to the crop as the organic matter is mineralized (decomposed) by soil organisms. Mineralization of organic matter and release of N increases as soil warms in the spring. When little N is available from animal manure, biosolids or legumes, the majority of the crop N requirement must be supplied by mineral fertilizer sources such as urea ammonium nitrate solution, urea, ammonium nitrate, or ammonium sulfate.
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Nitrogen behavior in the soil is difficult to predict because N transformations in soil are very complex (Figure 1). Over 98% of the N in most soils is unavailable for plant uptake at any specific time because it is fixed in soil organic matter or in clay minerals. Nitrogen in organic matter (e.g., plant residue, cover crops, animal manure, biosolids) may undergo microbial transformations that convert it to a plant-available form. The end result of this process is the NO3 form of N. The transformation rate of organic N to plant-available NO3 in the spring increases as the soil temperature increases, and much plant-available N can be produced from organic N in Virginia, beginning in mid-May in eastern Virginia to mid-June in western Virginia.
Soil testing in Virginia for available N before the growing season, as is practiced for other nutrients, does not accurately reflect the availability of N when it is most important to the crop (i.e., 30 to 45 days after emergence). The NO3-N soil test procedure relies on sampling and testing after the crop has emerged and grown for several weeks. The concentrations of soil NO3-N measured by this procedure are the result of many complex reactions affecting soil N and are more closely related to the need for supplemental N fertilization than any other procedure tested to-date.
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Data from 47 field research experiments conducted in the Coastal Plain, Piedmont, and Ridge and Valley soil provinces in Virginia during 1990 and 1991 demonstrated that corn grain yields were maximized (i.e., relative yield = 1.0, or 100% of maximum) at soil NO3-N concentrations above 18 parts per million (ppm) (Figure 3). Enough N was mineralized, or made available from decomposing organic N, at the locations where NO3-N concentrations were above 18 ppm to supply the seasonal N needs of the corn. Below 18 ppm, most of the relative yields were low, and supplemental N was needed to attain maximum yields. High relative yields occurred primarily where soil had received considerable contributions of organic N, such as from animal manures, biosolids, legume forages, or legume cover crops. Therefore, the PSNT should be utilized primarily on soils that have received significant amounts of organic N.
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These recommendations should not substitute for common sense and an understanding of the effects of soil properties and management practices on N availability to corn.
| NO3-N concentration | N rate recommendation |
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| < 10 ppm | Apply full rate of sidedress N that is needed for the realistic yield goal for the particular soil as specified by calculations from VALUES. |
| 10-20 ppm | Possible reduction of the normal sidedress N application by 25-50%. The decision to red uce the recommended N rate must be made on a site-by-site basis and should take into account previous field history, organic N additions, and management practices. |
| > 20 ppm | No sidedress N is needed. |
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Simpson, T.W., S.J. Donohue, G.W. Hawkins, M.M. Monnett, and J.C. Baker. 1993. The development and implementation of the Virginia agronomic land use evaluation system. Dep. of Crop and Soil Environmental Sci., Virginia Tech, Blacksburg, Virginia. 83 p.
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