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USDAAgricultural Research Service and Dep. of Agronomy, Univ. of Nebraska, Lincoln, NE 68583
* Corresponding author (gvarvel1{at}unl.edu)
Received for publication July 5, 2006.
| ABSTRACT |
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Abbreviations: GDD, growing degree days SI, sufficiency index
| INTRODUCTION |
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The differences in N-use efficiency, depending on crop yield identified above, demonstrate not only some of the problems in developing N recommendations for corn but also the complex interactions among the various factors to be considered. Stanford (1982) and Keeney (1982) provide excellent reviews of techniques for creating N recommendations based on laboratory incubations to estimate plant available N mineralized from organic matter and preplant soil tests to determine inorganic nitrate N. Laboratory incubation methods, inorganic nitrate N soil tests, and other procedures and techniques to determine N availability from other sources required to understand N management for crops are presented in a book edited by Hauck (1984). Chapters in the book present and discuss factors from N cycling in soil processes to N uptake by the crop affecting N-use efficiency in crop production. This book is just one example of the tremendous past effort by researchers to investigate, describe, and quantify N cycling processes to determine N available for crop production, this effort continues today.
In addition to the techniques described above, recent technological developments including global positioning systems, in-season real-time crop sensors, variable rate N applicators, and geographical information systems to analyze large amounts of data have improved our N recommendations. These developments continue to drive the expectation for further improvements in N management resulting in greater N application and use efficiency and producer profit while reducing surface and groundwater contamination.
In earlier reports, Varvel et al. (1997a, 1997b) demonstrated that chlorophyll meters provided excellent indications of in-season N status of several corn hybrids in both monoculture corn and soybeancorn cropping systems. In their reports, chlorophyll meter measurements taken throughout the growing season over several years indicated these data might have additional applications; including determination if and how much additional N fertilizer is needed for maximum yield. Therefore, our objective was to develop a plant-based technique to detect and correct N deficiencies during the cropping season with the ultimate purpose of improving N-use efficiency, maintaining or improving yield, reducing N fertilizer costs, and reducing environmental impacts of corn production.
| MATERIALS AND METHODS |
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Before initiation of the study, the site had been in a monoculture corn production system for more than 10 yr. At the beginning of the study, corn stalks from the previous growing season were shredded and the entire area was disked twice before planting. Similarly, each year following, corn stalks from both cropping systems were shredded and the entire area, including that which had been in soybean, was disked twice before planting.
A split-split-split plot treatment design within a randomized complete block experiment with four replications was used. Cropping systems were assigned as the main plots, corn hybrids as the subplots, and N fertilizer regimes as the sub-subplots. All phases of the monoculture corn and soybeancorn systems appeared each year starting with the 1991 growing season. Four Pioneer1 brand corn hybrids (3162, 3379, 3394, and 3417) differing in yield potential and maturity were selected and used in both the monoculture and rotation systems from 1991 through 2000. In subsequent years, new corn hybrids with similar growth characteristics and maturity groups were selected to replace the four original hybrids. For 2001 and 2002 they were Pioneer brand hybrids (32R42, 33B50, 33G26, and 33P66) and for 2003 and 2004 they were Pioneer brand hybrids (31N27, 33B50, 33V15, and 33P66). All corn hybrids were planted between late April and mid-May in 8-row (91-cm row spacing) by 15.2-m long plots at approximately 74000 seeds ha1. Soybean in the soybeancorn rotation was planted in early to mid-May. Except for N fertilizer application rates, both corn and soybean were produced using production practices typical to the area.
Nitrogen fertilizer as NH4NO3 was broadcast and immediately incorporated with a 6- to 7-mm sprinkler irrigation in early June when corn was at approximately V2 or V3 growth stages (Ritchie et al., 1986). Six fertilizer N regimes including five fixed N fertilizer rates (0, 50, 100, 150, and 200 kg N ha1) and one "as needed" rate (Varvel et al., 1997a) were used on both crops. Only data from the fixed rate treatments were used for this analysis. Irrigation was provided as needed with a linear-drive sprinkler system.
In-season corn N status was monitored in both cropping systems using Minolta SPAD 502 chlorophyll meters (Peterson et al., 1993) starting at the V8 growth stage and continuing through R2 (Ritchie et al., 1986). Chlorophyll meter readings were taken from the uppermost fully expanded leaf (collar visible) until the VT growth stage. After VT, meter readings were collected from the ear leaf. All measurements were taken on 30 randomly selected plants within each plot using the procedure described by Blackmer et al. (1993).
Chlorophyll meter readings were analyzed by sampling date each year. As noted in earlier publications (Varvel et al., 1997a, 1997b), chlorophyll meter readings and grain yields responded similarly to N fertilizer applications and chlorophyll meter readings were an excellent indication of N sufficiency or deficiency in irrigated corn. Actual SPAD readings were normalized to adjust for variation not associated with N nutrition. The SPAD readings from all treatments were divided by the maximum reading from all N rates within that cropping system, hybrid, and replication within each date and year to obtain a sufficiency index (SI), which is expressed as a decimal (Peterson et al., 1993).
Chlorophyll meter data were collected at various sampling dates each year over the 10 yr of the study. Combining the data over years required computation of thermal times (growing degree days, GDD) for each of the dates chlorophyll meter data were collected. Thermal time computations were made using Method II of McMaster and Wilhelm (1997). In Method II computations, daily maximum (TMAX) and minimum (TMIN) temperatures, a base (TBASE) temperature of 10°C, and a threshold (TTHRESH) temperature of 30°C are used. Then GDD = [(TMAX + TMIN)/2] TBASE with the following conditions: If TMAX < TBASE, then TMAX = TBASE, if TMIN < TBASE, then TMIN = TBASE, if TMIN > TTHRESH, then TMIN = TTHRESH, and if TMAX > TTHRESH, then TMAX = TTHRESH. These substitutions are made before calculating (TMAX + TMIN)/2.
Final grain yield was determined with a plot combine by harvesting three interior rows for the entire length of each plot. Yield data were adjusted to 155 g kg1 moisture. Grain yield data were also normalized by dividing each yield by the maximum yield from all fixed N fertilizer rate treatments within that cropping system, hybrid, and replication to obtain a relative grain yieldanalogous to the computation above of SI for chlorophyll meter readings.
Data from the study were analyzed both within and across cropping systems using regression analyses to determine whether responses to applied N fertilizer were significant. Four response models (quadratic, quadratic-plus-plateau, exponential, and square root) were fit to SI and normalized grain yield data using the NLIN procedure in SAS (Ihnen and Goodnight, 1985). All statistical analyses were performed using PC Version 9.1 of the Statistical Analyses System for Windows (SAS Institute, 2003).
| RESULTS AND DISCUSSION |
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Corn grain yields in the monoculture corn system ranged from 3.50 to 13.63 Mg ha1 during the 10 yr of the study (Fig. 1 ) and significant responses to the applied N fertilizer were obtained every year. It is apparent that although maximum grain yields varied from year to year (ranging from a low of 10.44 Mg ha1 in 1995 to a high of 13.63 Mg ha1 in 2004), in most years maximum yield occurred between the 150 and 200 kg N ha1 rate (Fig. 1). Regression analyses performed on these data, combined over years, using a quadratic response model indicated the maximum yield occurred at 174 kg N ha1 for this site. For each year individually, regression analysis indicated maximum grain yield occurred within 10 kg N ha1 of the 174 kg N ha1 in all years except 1995 (140 kg N ha1) and 2004 (200 kg N ha1). This result supports conclusions from research by Blackmer et al. (1997) in Iowa, Fox and Piekielek (1995) in Pennsylvania, Kachanoski et al. (1996) in Ontario, Canada, Mulvaney et al. (2006) in Illinois, and Vanotti and Bundy (1994) in Wisconsin, that contradict the yield goal method for making N fertilizer recommendations for corn. This method has relied on a yield goal based system that assumes a constant factor of 19.4 to 24.2 kg N Mg1 of grain, multiplied by the expected yield goal to generate the basic N application recommendation (Mulvaney et al., 2006). Using this approach with actual maximum yields from each individual year for the results from our multiyear study would have produced different N fertilizer recommendations calculated across years ranging from a low of 203 kg N ha1 in 1995 to a high of 264 kg N ha1 in 2004 (using the more conservative 19.4 kg N Mg1 factor). Obviously if the greater factor, 24.2 kg N Mg1 grain were used, the magnitude and range of N fertilizer recommendations would be greater. Even if we used the average maximum yield over the 10-yr period, 12.1 Mg ha1, 235 kg N ha1 would have been recommended on an annual basis. All of these recommendations are much higher than the 174 kg N ha1 indicated by solving for the maximum of the quadratic response function describing the data in Fig. 1. These results support the fact that factors other than, or in addition to, amount of available N determines fluctuations in maximum corn grain yields from year to year. Some of these factors are rainfall amount and seasonal distribution, soil water conditions, thermal time accumulation patterns, total incoming and intercepted radiation, dates of planting, and intensity of pests and diseases.
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Determination of N deficiencies at the earliest possible time in the growing season (earliest stage of crop development) will increase a producer's opportunity and potential ability to correct that deficiency. Chlorophyll meter data were consistently available in all years at or near 450, 560, and 670 GDD, corresponding approximately to V8, V10, and V12 growth stages (Ritchie et al., 1986), respectively. Analyses of data collected at these times from the monoculture corn system were used to determine how early in the season chlorophyll meter data could be used to predict future crop N need, how much N was needed, and if analyses based on data collected later in the season improved the accuracy of predicted N need.
As noted above, Varvel et al. (1997a, 1997b) demonstrated N fertilizer significantly increased both corn grain yield and chlorophyll meter readings in this study. Since the specific grain yield response to applied N varied from year to year (Fig. 1), yield data were normalized by dividing each yield by the maximum yield from all fixed N fertilizer rate treatments within that cropping system, hybrid, and replication to obtain a relative grain yield (Fig. 2 )analogous to the computation of SI for chlorophyll meter readings. Linear correlations between relative grain yield and SI at the three times (450, 560, and 670 GDD) each year across the 10 yr of the study indicated the variables were highly related and that normalized yield and SI responded similarly to N fertilizer (Table 1).
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Quadratic models for the three observation times (at 450, 560, and 670 GDD) had intercepts and linear and quadratic coefficients similar in magnitude (Table 2). However when compared using contrast statements in regression analyses, they were determined to be statistically different. This outcome is not surprising considering the large number of degrees of freedom in the analyses (N = 800). All three equations reached a maximum SI at about 170 kg N ha1, similar to the 174 kg ha1 N rate found from regression of N rate and maximum grain yield from data in Fig. 1. These results, and the relative similarity of the equations, indicated chlorophyll meter-based SI values throughout much of vegetative growth for corn were fairly stable. Based on this premise, we felt it was appropriate to combine data from all three thermal times and fit a single quadratic model to test its appropriateness for use across the vegetative phase (Table 2). As would be expected, this model was very similar to the models from the individual thermal times, with the intercept and linear and quadratic coefficients intermediate to those describing the SI response at each individual thermal time (Table 2). Again, given the exceptionally large number of degrees of freedom available (N = 2400), when this equation was compared to the three separate equations using an F test, it was found to be significantly different. In spite of statistical procedures, the combined quadratic model appeared similar to the individual equations obtained at the three thermal times, and it seemed plausible that it could be used to represent the relationship between SI and N fertilizer rates throughout the vegetative growth period.
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Logically, a question arises as to whether this model is specific to monoculture corn. Because the relationship is built on in-season assessment of canopy N status, all sources and uses of N by the crop and other components of the N cycle are accounted for and N availability is "reported" by the plant. We believe the model is valid beyond its conditions of development, monoculture corn. Earlier research indicated corn following soybean at this location required less preplant fertilizer (65 kg N ha1 yr1 less) for maximum grain yields than in the monoculture corn system (Varvel and Wilhelm, 2003). In addition, maximum grain yields were generally greater for the soybeancorn system than for the monoculture corn system (Varvel and Wilhelm, 2003). To test our supposition, SI data collected from the soybeancorn system for all three thermal times (2400 additional observations) was combined with the data from the monoculture corn system and analyzed as described above. The optimum N fertilizer rate for maximum SI (176 kg N ha1) was almost identical to that for the monoculture corn system, demonstrating our model's robustness and applicability in other cropping situations with varying amounts of available N early in the growing season. This analysis also demonstrated that even though the magnitude of N response was much less in the soybeancorn system, the response curves maximums were similar. Since the magnitude of response was less, it was also obvious that SI values in the soybeancorn system were much greater, indicating that less additional N fertilizer would need to be added for maximum grain yields. As we had postulated above, by monitoring the plant we were able to give credit for the additional N available to corn following soybean.
| CONCLUSIONS |
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This general approach should be valid regardless of the instruments used to acquire data for SI. The only requirements are that the instrument readings respond to N rate and they are related to yield. These limitations are quite reasonable and should allow the approach to be used with the array of on-the-go sensors under development at this time. Wide-area use of modern sensors and this method of assessing the amount of N needed to maximize yield will reduce application of N in excess of crop need while maintaining high yield levels required for profitable grain production enterprises.
| ACKNOWLEDGMENTS |
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| NOTES |
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1 Trade names and company names are included for the benefit of the reader and do not imply any endorsement or preferential treatment of the product by the authors, USDAAgricultural Research Service, or the Agricultural Research Division of the University of Nebraska. ![]()
| REFERENCES |
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