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Effects of both above and below ground biomass on soil chemical, physical and biological properties on a coastal plain soil in North Carolina .

机译:北卡罗莱纳州沿海平原土壤上,地下生物量对土壤化学,物理和生物学特性的影响。

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摘要

The literature has shown the possibility to enhance many of the soil properties that improve production with additions of plant biomass to the soil in conjunction with long-term conservation tillage. Since it has been proven that reduced tillage is extremely beneficial to a soil's health, the key question is if the incorporation of deep rooted cover crops and/or large quantities of above ground biomass over a two-year period would result in extensive improvements on a soil's natural properties throughout the effective rooting depth, or is this too short of a time period for any beneficial effects to occur to the chemical, physical and biological properties of the soil? While SOC additions to the soil surface through decaying biomass can make measurable improvements to a soil in the humid, tropical southeastern U.S., the dynamics of total carbon (total SOC), total nitrogen (TKN), particulate organic matter (POM), potentially mineralizable nitrogen (PMN), CEC and bulk density (Db) in the 0--5, 5--10, and 10--18 cm depths in a production system that incorporates deep rooted cover crops and/or additions of organic matter from cover crops at rates >6 Mg/ha/yr (3 T/ac) are unknown. The objectives of this research were to determine what effect rye ( Scale cereale), barley (Hordeum vulgare), alfalfa (Medicago sativa), wheat (Triticum aestivum), triticale (Triticale hexaploide Lart.), annual white sweetclover (Melilotus officinalis), blue lupine (Lupinus angustifolius ), rye/hairy vetch (Scale cereale/Vicia villiosa) and alfalfa/rye (Medicago sativa/Scale cereale) would have on the following parameters: total SOC, POM, TKN, PMN, CEC, and Db after two (2) years of seeding. Significant spatial/temporal interactions and main effects were found in Db, PMN, POM and CEC while significant main effects were found in total C and total N. Significant treatment interactions were found in Db, total C, PMN, POM and CEC. Relative to treatment biomass, significant effects were seen between treatments and treatment*year interaction. Results on Db found spatial variability with depth but not with season and a minimal treatment effect depending on surface texture. Total C and total N decreased with depth but were independent spatially and temporally; however, treatment effect on total C was 5 months. Between Db and total C, the two parameters were inversely correlated. PMN either fluctuated between sampling times or declined with time. Notably, rye and rye/hairy vetch effected PMN in the 0--5 cm depth where other treatments showed no effect. POM declined with time regardless of depth implying a priming effect was occurring; however, rye/hairy vetch appeared to show an early reversal trend. As for CEC, there was no consistent trend. Additionally, CEC exhibited a moderate correlation to POM but not total C. Biomass measurements indicated no treatment consistently exceeded >6 Mg/ha/yr. Rye and rye/hairy vetch more often produced the most biomass and lupine achieved the overall maximum yield. Relationships between biomass and N parameters found a moderate, positive effect from the biomass inputs that appeared to compound with time. Overall, rye and rye/hairy vetch were the best cover crop treatments but two years of biomass inputs were not enough to prevent declines in POM. Conversely, PMN fluxed from applied N, and biomass with low C:N ratios oxidized quickly resulting in less carbon. Total C, total N and Db were not responsive to short term management indicating more effort is needed to define and/or develop a cover crop that will consistently reach the >6 Mg/ha/yr.
机译:文献已经表明,通过向土壤中添加植物生物量以及长期的耕作耕作,可以提高许多土壤特性,从而改善产量。由于已经证明减少耕作对土壤健康极为有益,因此关键问题是,如果在两年内掺入根深蒂固的覆盖作物和/或大量地上生物量,是否会在耕作上带来广泛的改善在整个有效生根深度中土壤的自然特性,还是这个时间太短,以至于不会对土壤的化学,物理和生物学特性产生任何有益影响?尽管通过降解生物量向土壤表面添加SOC可以使美国东南部潮湿,热带的土壤得到可测量的改善,但总碳(总SOC),总氮(TKN),颗粒有机物(POM)的动态变化,可能会矿化生产系统中深度为0--5、5--10和10--18厘米的氮(PMN),CEC和体积密度(Db),其中包括深根覆盖的农作物和/或从覆盖物中添加的有机物目前尚不清楚农作物的生长速率> 6 Mg / ha / yr(3 T / ac)。这项研究的目的是确定黑麦(Scale谷物),大麦(Hordeum vulgare),苜蓿(Medicago sativa),小麦(Triticum aestivum),小黑麦(Triticale hexaploide Lart。),一年生白三叶草(Melilotus officinalis),蓝色羽扇豆(Lupinus angustifolius),黑麦/多毛etch子(Scale谷类/野豌豆)和苜蓿/黑麦(Medicago sativa / Scale谷类)具有以下参数:总SOC,POM,TKN,PMN,CEC和Db两(2)年播种。在Db,PMN,POM和CEC中发现了显着的时空相互作用和主要效应,而在总C和总N中则发现了显着的主要效应。在Db,总C,PMN,POM和CEC中发现了显着的治疗相互作用。相对于处理生物量,在处理与处理*年度交互之间可看到显着效果。 Db的结果发现,深度随深度而变化,而随季节而变化,并且根据表面纹理的不同,处理效果最小。总碳和总氮随深度而降低,但在空间和时间上独立。但是,治疗对总C的影响小于5个月。在Db和总C之间,两个参数成反比。 PMN在采样时间之间波动或随时间下降。值得注意的是,黑麦和黑麦/多毛v子在0--5 cm深度影响PMN,其他处理均无效果。 POM随时间而下降,无论深度是否暗示有引发作用。然而,黑麦/毛v子似乎表现出早期逆转趋势。对于CEC,没有一致的趋势。此外,CEC与POM呈中等程度的相关性,但与总C无关。生物质测量表明,没有任何一项处理始终超过> 6 Mg / ha / yr。黑麦和黑麦/多叶紫etch的生物量最高,羽扇豆的总产量最高。生物量和N参数之间的关系从似乎随着时间复合的生物量输入中发现了适度的积极影响。总体而言,黑麦和黑麦/有毛v子是最好的覆盖作物处理方法,但是两年的生物量输入不足以防止POM下降。相反,PMN从施加的氮中逸出,低C:N比的生物质被快速氧化,从而减少了碳含量。总C,总N和Db对短期管理没有反应,表明需要更多的努力来确定和/或开发将持续达到> 6 Mg / ha / yr的覆盖作物。

著录项

  • 作者

    West, Eric Wayne.;

  • 作者单位

    North Carolina State University.;

  • 授予单位 North Carolina State University.;
  • 学科 Agriculture Agronomy.;Agriculture Soil Science.
  • 学位 Ph.D.
  • 年度 2010
  • 页码 109 p.
  • 总页数 109
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:37:03

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