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A conceptual model to estimate the nitrogen requirement of corn (Zea mays L.)Lopez Collado, Catalino Jorge 25 April 2007 (has links)
The objectives of this work were to evaluate the vegetative parameters used to estimate crop N demand and to estimate the accuracy and precision of the conceptual model of fertilization using an error propagation method. Corn plants were collected throughout the entire crop life cycle to determine the fresh and dry weight of the aboveground biomass and roots, root index, plant height, and corn grain yield. Three experiments were conducted, two under field conditions and one under greenhouse conditions. In the first field experiment in 2002, three sites were selected. The first site was the Texas A&M University (TAMU) Agricultural Experiment Station Research Farm in which a Ships clay soil was used. The second site was a cooperative farmer's land on a Weswood silt loam soil in Burleson County. These first two sites used Pioneer 32R25 as the corn hybrid. The third site was also a Ships soil in the TAMU Farm, but Dekalb 687 was the corn variety. In 2003, the second experiment was on a Ships soil in the field of TAMU Farm, and the third experiment was conducted in a greenhouse using Ships and Weswood soil. No differences in the root index and harvest index were observed, even when the Dekalb 687 hybrid was included. Variations in plant N concentration, moisture content, and yield were noted, but followed predictable patterns with time over the season. These parameters were consistent throughout the entire life cycle of the crop. The linear relationship between the fresh weight of aboveground biomass and fresh weight of roots was R2 = 0.92, the moisture content of corn plants over time was fit to a second grade polynomial with R2 = 0.98, and plant N content had a close linear relationship (R2=0.90) with the total plant dry weight, including roots, at harvest. The accuracy of the conceptual model was low under field conditions (55%), but high under greenhouse conditions (90%). Precision of the conceptual model was low both in the field (194%) and the greenhouse (115%) conditions.
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Investigating 55 years of nitrogen loading to the Chesapeake Bay using the HSPF modelLepp, Marinna. January 2009 (has links)
Thesis (M.A.S.)--University of Delaware, 2009. / Principal faculty advisor: Dominic M. Di Toro, Dept. of Civil & Environmental Engineering. Includes bibliographical references.
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Residual soil nitrogen and nitrogen response of corn after alfalfa on sandy loam soil /Pearson, William W. January 2002 (has links) (PDF)
Thesis (M.S.)--University of Wisconsin--Stevens Point, 2002. / Includes bibliographical references (leaves 69-75).
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ISOTOPIC NITROGEN FIXATION BY DESERT ALGAL CRUST ORGANISMSMayland, H. F. (Henry F.) January 1965 (has links)
No description available.
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Effects of nitrogen sprays on the growth of lettuceFazio, Steve, 1916- January 1951 (has links)
No description available.
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Soil nitrogen fractions and their relationship to nitrogen fertilizer yield response and nitrogen uptake of Sudan-Sorghum hybrid grass on twenty Quebec soils.Kadirgamathaiyah, Simathamby. January 1967 (has links)
No description available.
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Studies on the nitrogenous constituents of brewers spent grainCrowe, Nancy (Nancy Lynn) January 1983 (has links)
No description available.
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The reaction of active nitrogen with oxygen.Vlastaras, Athanasios S. January 1966 (has links)
No description available.
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Microbial response to nitrogen availability : preferential and adaptive community uptakeBunch, Nathan D. January 2010 (has links)
This project was designed to assess the ability of natural sediment microbial communities and single species microbial populations to preferentially utilize inorganic forms of nitrogen (ammonium, NH4-N, and nitrate, NO3-N, specifically). The first chapter addressed two primary questions: 1) Do sediment microbial communities preferentially assimilate NH4-N or NO3-N?; and, 2) Does preferential uptake of nitrogen change with increased NH4-N or NO3-N availability? The second chapter furthered these analyses by assessing shifts in microbial nitrogen assimilation in response to sustained nitrogen enrichments. Primary questions addressed were: 1) Are microbial communities able to adapt to nitrogen enrichment and preferentially utilize a more available source?; and, 2) Are initial microbial responses to nitrogen enrichment different from sustained responses? Questions were addressed with in vitro laboratory experiments quantifying microbial activity. Overall, microbial community activity changed in response to the form of nitrogen available, enrichment type, and duration of exposure. Data demonstrate sediment microbial communities in the Midwestern US may prefer NO3-N over other forms of nitrogen. However, microbial communities became saturated with NO3-N with increases in concentrations >0.75 mg NO3-N/L. Microbial communities were able to adapt to higher nitrogen concentration and increase rates of assimilation for both NH4-N and NO3-N. Thus, microbial communities are robust in response to nitrogen increases in and ecosystem, even in high nitrogen environments like the Midwestern US. / Preferential uptake of available nitrogen forms -- Adaptive uptake in microbial communities. / Department of Biology
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The effect of time and rate of nitrogen fertilization of corn on the nitrogen balance in some Quebec soils.Sadler, John M. January 1967 (has links)
No description available.
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