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Title:
Improved Nitrogen Fertilizer Recommendations for Soils Incorporating a Simple Measurement of Soil Physical Properties

Investigators:
Peter Motavalli and Stephen Anderson
Department of Soil and Atmospheric Sciences, University of Missouri-
Columbia, 302 ABNR Bldg, Columbia, MO 65203

Objectives:

  1. To determine the relationship between nitrogen (N) fertilizer efficiency in corn and several soil physical properties (i.e. soil structure, soil moisture retention, and water infiltration) in claypan soils.
  2. To develop a simple and quick routine procedure to estimate soil physical properties that may improve N fertilizer recommendations.
  3. To evaluate methods to include measurement of soil physical properties as a factor in adjustment of N fertilizer recommendations.

    Procedures:

    Field Experiment

    • A two-year field trial planted to corn (Zea mays. L.) will be established at the Bradford Agronomy Center in which 2 levels of surface compaction will be imposed (0, 2x passes of a tractor-pulled filled 500 gallon water tank) and 4 rates of N fertilizer (0, 75, 150, 225 lbs N/acre as ammonium nitrate) broadcast applied pre-plant in a factorial design. Treatments will have 4 replications and will be repeated each year. ·
    • The fate of applied fertilizer N will be monitored by periodic soil sampling and determination of NH4+-N and NO3--N in the soil profile. Changes in soil bulk density, water infiltration and soil moisture content will be measured periodically over the growing season and soil moisture release characteristics determined from intact soil cores taken from each plot. ·
    • Relative crop recovery of applied fertilizer N will be determined by N analysis of ear leaf samples, determination of crop yields, and N analysis of corn grain and forage among the treated plots.
    Laboratory Experiment
    • · Several low-cost and rapid procedures will be compared to determine their effectiveness in assessing soil physical properties for routine soil sampling. These methods will be tested in the range of soil physical properties imposed in the field experiment and compared to conventional measurements of soil bulk density, water infiltration and soil moisture content. The methods tested will include several types of portable penetrometers (pocket-type, electronic, and mechanical) and a rapid method to test water infiltration (single-ring method). ·
    • Possible methods to incorporate measurements of soil physical properties in Missouri N fertilizer recommendations will be evaluated based on results from the field trial and other available research in the state. These methods may include a modifier that reduces yield goals in soils with physical restrictions or an index that increases or decreases N fertilizer recommendations based on observed changes in N fertilizer efficiency with increasing physical restrictions.

      Current Status and Importance of Research:

      Natural and induced soil physical restrictions to crop growth are a common problem in Missouri soils. These restrictions include claypans, tillage pans, fragipans and compacted soil layers. Soil physical properties affect several soil processes including the rate of water infiltration into soil, soil moisture availability to plants, and nutrient transformations. Due to the importance of soil physical properties for root growth in Missouri soils, Scrivner et al. (1985) developed a soil productivity index for Missouri that included measurements of potential available water capacity (a property related to soil texture), bulk density and soil pH by depth to predict root growth.

      Reduction in agricultural production due to physical restrictions, such as soil compaction, has been attributed to poor soil aeration, the high penetration resistance of compacted soils to root growth, and increased nutrient losses (Hillel, 1980). Soil physical properties that increase soil moisture may also reduce rates of N mineralization due to increased anaerobic conditions. Additional negative effects of processes affected by soil physical properties, such as soil compaction, are increased potential for environmental contamination due to reduced water infiltration and increased surface runoff, soil erosion, and transport of agricultural chemicals and nutrients in runoff to aquatic systems (Håkansson and Voorhees, 1997).

      Although crop yield potential may be reduced in soils with physical restrictions, current N fertility recommendations from the University of Missouri for agronomic crops do not account for the effects of soil physical properties on crop production. In fact, research has shown that non-sandy Missouri soils with bulk densities greater than 1.3 g cm-3 have reduced potential productivity for crop growth (Scrivner et al., 1985). Among the current factors affecting N fertilizer recommendations are type of crop, yield goal, and soil organic matter content. A better understanding of the relationships between soil physical properties, fertilizer N efficiency and yield of field corn will assist in developing improved fertilizer management practices for soils with physical restrictions, such as higher or lower N fertilizer rates, and changes in fertilizer placement and timing of application. In addition, quantification of yield reductions due to soil physical restrictions will aid producers in management decisions.

      Timetable:


      Plant experiments
      April, 2001 Apply and establish N fertilizer and compaction treatments
      April-Sept., 2001 Sample and analyze soil and plant tissue
      Test soil physical assessment methods
      Sept./Oct, 2001 Harvest experiments and sample and analyze soil and plant tissue
      November, 2001 Analyze research results
      December, 2001 Annual report
      April-Nov. 2002 Same as 2000
      December 2002 Submit final report

      Expected Benefits and Strategy for Application/Transfer of Knowledge:

      The addition of an assessment of soil physical restrictions in calculating N fertilizer recommendations will improve N fertilizer management and provide growers with important information to manage a major soil physical factor that limits crop yield. This proposed project will also increase our knowledge of the fate of N fertilizer applied to claypan soils with physical restrictions. Additional information will be developed for the potential use of rapid and inexpensive methods to assess soil physical properties. It is anticipated that including soil physical properties as a factor in N fertilizer recommendations for Missouri will require additional calibration and testing for the major soil types around the state.

      The results of this project will be incorporated into research and extension publications and workshops. A graduate student will receive support under this grant for their graduate dissertation research training.

      References

      Håkansson, I. and W.B. Voorhees, 1997. Soil compaction. p. 167-179. In R. Lal, W.H. Blum, C. Valentine and B.A. Stewart (eds.) Methods for assessment of soil degradation. CRC Press, Boca Raton, FL.

      Hillel, D. 1980. Fundamentals of soil physics. Academic Press, San Diego, CA.

      Scrivner, C.L., B.L. Conkling, and P.G. Koenig. 1985. Soil productivity indices and soil properties for farm-field sites in Missouri. Agricultural Experiment Station, University of Missouri-Columbia, Columbia, MO.

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