首页> 外文学位 >CHARACTERIZATION OF DENITRIFICATION AND LEACHING LOSSES OF FERTILIZER NITROGEN FROM SOIL (EVOLUTION, ISOTOPE, NITROUS OXIDE, DINITROGEN).
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CHARACTERIZATION OF DENITRIFICATION AND LEACHING LOSSES OF FERTILIZER NITROGEN FROM SOIL (EVOLUTION, ISOTOPE, NITROUS OXIDE, DINITROGEN).

机译:土壤中脱氮的特征和肥料氮的淋失(演变,同位素,一氧化二氮,双氮)。

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摘要

Quantification of leaching and denitrification losses of fertilizer N from soil requires that appropriate methods be developed for their measurement. The objectives of this work were to: (1) evaluate potential errors in measuring denitrification by use of ('15)N-tracer techniques recently developed for determination of N(,2) and N(,2)O evolved from soil; (2) evaluate three methods of estimating fertilizer N loss under field conditions (grain yield reductions, an ('15)N difference method, and a direct measurement of denitrification using the procedures in 1); and (3) evaluate the extent of N loss through leaching and denitrification in a laboratory study using semi-disturbed soil columns.;The ('15)N difference study was conducted to determine the amount of fertilizer N loss that would occur from ambient rainfall (0-cm addition) and ambient rainfall plus 7.6 cm of additional water (7.6-cm addition). Of the 168 kg N/ha applied, 141 and 104 kg N/ha were accounted for at harvest for the 0 and 7.6-cm water additions, respectively. Gas analyses accounted for losses of 24 and 44 kg N/ha, respectively, with very little leaching occurring for either treatment. Essentially all of the N loss occurred by the time of the 11-leaf growth stage. The yield study indicated that average corn (Zea mays L.) yield reductions across N rates of 0-224 kg N/ha were great enough to justify application of supplemental N. Using yield as a measure of N loss provided larger estimates than either the ('15)N difference method or gas analyses.;The soil column study included water and fertilizer treatments similar to those used in the field study. Nitrogen evolution amounted to only 1 kg N/ha for the highest water treatment. A separate investigation indicated C availability was apparently limiting denitrification despite the addition of plant residue. The reason for the discrepancy between large N evolution rates under field conditions and small losses under laboratory conditions was not evident.;Computer simulation studies showed that when nitrate undergoing denitrification is not isotopically uniform, N evolution rates will be underestimated. The degree of error increases with an increase in the number of NO(,3)('-) pools present where their isotopic diversity increases (range or standard deviation of the ('15)N enrichments). The error will generally not exceed 25% where the ('15)N enrichments are low (<40 atom %). Where the enrichments remain high (>40 atom %), the error generally will not exceed 10%.
机译:量化土壤中肥料N的淋溶和反硝化损失需要开发出适当的测量方法。这项工作的目的是:(1)使用最近开发的用于确定从土壤中释放出来的N(,2)和N(,2)O的('15)N-示踪剂技术,评估反硝化测量中的潜在误差; (2)评估估算田间条件下肥料氮损失的三种方法(降低谷物产量,采用('15)N差异法,以及使用1中的步骤直接测量反硝化作用); (3)在使用半扰动土壤柱的实验室研究中,通过淋洗和反硝化作用来评估氮素损失的程度。(15)氮差异研究旨在确定由于环境降雨而导致的肥料氮素损失量(附加0厘米)和周围的降雨加上7.6厘米的附加水(附加7.6厘米)。在施用的168千克氮/公顷中,添加0和7.6厘米水时分别占141和104千克氮/公顷。气体分析分别造成24和44 kg N / ha的损失,两种处理的浸出很少。基本上所有的N损失都在11叶生长期发生。产量研究表明,在0-224 kg N / ha的氮肥水平下,平均玉米(Zea mays L.)产量的降低足以证明补充氮肥的使用是合理的。 ('15)N差异法或气体分析。;土壤柱研究包括与田间研究相似的水和肥料处理。对于最高的水处理,氮释放量仅为1 kg N / ha。一项单独的研究表明,尽管添加了植物残渣,但C的可用性显然限制了反硝化作用。田间条件下大氮的释放速率与实验室条件下小氮损失之间存在差异的原因尚不明确。计算机模拟研究表明,当硝酸盐进行反硝化作用时同位素分布不均匀时,氮的演化速率将被低估。错误的程度随其同位素多样性增加((15)N富集的范围或标准偏差)的NO(,3)('-)库数量的增加而增加。当('15)N富集度较低(<40原子%)时,误差通常不会超过25%。在富集度保持较高(> 40原子%)的情况下,误差通常不会超过10%。

著录项

  • 作者单位

    University of Illinois at Urbana-Champaign.;

  • 授予单位 University of Illinois at Urbana-Champaign.;
  • 学科 Agriculture Agronomy.;Chemistry Agricultural.
  • 学位 Ph.D.
  • 年度 1986
  • 页码 99 p.
  • 总页数 99
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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