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Impact of crop and residue management on the physical and chemical stabilization of soil organic matter at farm level.

机译:作物和残留物管理对农场一级土壤有机质的物理和化学稳定的影响。

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摘要

This dissertation explores changes over time in soil organic matter (SOM) stabilization of two irrigated production fields: a continuous maize sequence that was converted from no-till to conservation deep tillage (Site 1), and a no-till maize-soybean rotation (Site 2). An integrated approach using humic acid extractions and density-based physical fractionation of SOM within aggregate size classes was developed to evaluate the changes in SOM stabilization (physical protection, organo-mineral associations and humification). At Site 1, loss of SOM in the surface layer was compensated for by increased SOM in deeper soil layers with no net change in C stocks. Whole field C-stocks in the 0-400 kg soil m-2 layer of Site 1 were 7.09 +/- 0.29, 7.47 +/- 0.36, 7.15 +/- 0.37 and 7.18 +/- 0.41 kg C m -2 in fall of 2005, 2006, 2007 and 2008, respectively. This outcome is encouraging, given the challenge of stabilizing aboveground residues into the mineral matrix without increasing tillage-induced C losses from native SOM and residues due to enhanced decomposition. At Site 2, there was an increase in C and N stocks in surface soil after the second maize year (2007). Whole field C stocks in the 0-400 kg soil m-2 layer of Site 2 were 6.42 +/- 0.30, 6.18 +/- 0.32, 6.81 +/- 0.26 and 6.72 +/- 0.29 kg C m-2 in fall of 2005, 2006, 2007 and 2008, respectively. The changes in soil 13C signature and monosaccharide composition, together with changes in SOM fraction amount support a large input of soybean residues as key to promote stabilization of standing maize litter through physical protection and humification. Preferential SOM accumulation in the largest, most C-enriched aggregates was associated with less humified SOM fractions while similar accumulation rates of more humified fractions were found among aggregate classes. These findings support stabilization of crop residues as SOM under high yield maize and soybean management at field scale.
机译:本文探讨了两个灌溉生产田的土壤有机质(SOM)稳定性随时间的变化:从免耕到保护性耕作的连续玉米序列(站点1),以及免​​耕玉米-大豆轮作(网站2)。开发了一种使用腐殖酸提取和基于SOM的基于密度的物理分级在集料尺寸类别中的集成方法来评估SOM稳定性的变化(物理保护,有机矿物质的缔合和腐殖化)。在站点1,表层SOM的损失被深层土壤中SOM的增加所补偿,而C量没有净变化。站点1的0-400 kg土壤m-2层中的全田C储量秋季下降为7.09 +/- 0.29、7.47 +/- 0.36、7.15 +/- 0.37和7.18 +/- 0.41 kg C m -2分别为2005、2006、2007和2008年。考虑到将地上残留物稳定在矿物基质中的挑战,而又不增加耕种引起的天然SOM和由于增强分解而产生的残留物造成的C损失,这一结果令人鼓舞。在第二个玉米年度(2007年)之后,表2的表层土壤中的C和N储量有所增加。站点2的0-400 kg土壤m-2层中的全田C储量在秋季下降时分别为6.42 +/- 0.30、6.18 +/- 0.32、6.81 +/- 0.26和6.72 +/- 0.29 kg C m-2 2005、2006、2007和2008。土壤13 C标记和单糖组成的变化,以及SOM分数的变化,支持大量的大豆残留物输入,这是通过物理保护和增湿作用促进玉米直立凋落物稳定的关键。在最大,最富C的聚集体中,优先SOM积累与较少腐殖质的SOM馏分相关,而在聚集体类别中发现较高腐殖分的相似积累率。这些发现支持了在高产玉米和大豆田间管理下作物残渣作为SOM的稳定化。

著录项

  • 作者

    Wingeyer, Ana Beatriz.;

  • 作者单位

    The University of Nebraska - Lincoln.;

  • 授予单位 The University of Nebraska - Lincoln.;
  • 学科 Agriculture Agronomy.;Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 229 p.
  • 总页数 229
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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