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Plant responses to increased experimental nitrogen deposition in a boreal peatland.

机译:植物对北方泥炭地中试验性氮沉积增加的反应。

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摘要

Increased nitrogen (N) deposition onto boreal peatlands and forests is anticipated with further expansion of Alberta's oil sands industry and consequently, an increase in sources of nitrogen oxide emissions. Increased N deposition has the potential to affect peatland flora and alter N cycling patterns in peatlands, therefore it is imperative to investigate at what level of excess N deposition these effects take place. This thesis discusses results from the first two years of a five year N fertilization study being conducted at a peatland complex near the hamlet of Mariana Lake in northeastern Alberta, Canada aimed at quantifying the N "critical load" for these peatland ecosystems. At the study site there are forty-two experimental plots -- half in an ombrotrophic bog, the other half in the poor fen -- with varying N fertilization treatments ranging from 0 kg/ha/year to 25 kg/ha/year. To investigate nitrogen uptake by plants at the Mariana Lake study site, I measured nitrogen (N) and carbon (C) concentrations of Sphagnum capitulum tissue and vascular plant foliar tissue. For Sphagnum species, I also analyzed C:N ratios and capitulum N storage. To investigate potential growth response of the target Sphagnum species, measurements were taken for linear growth (the vertical elongation of the Sphagnum shoots), stem mass density (the weight of Sphagnum stems occupying a volume after capitula were removed), and ultimately, net primary production (the product of the prior two measurements). Capitulum mass density (biomass) was measured as well to investigate possible changes in Sphagnum capitulum growth. Also, during the height of the growing season (mid-July, 2011 and 2012), the plant communities in each treatment plot were sampled to provide "baseline" data necessary for documenting any shifts in plant distribution or community composition that may occur after N additions.
机译:随着艾伯塔省油砂产业的进一步扩大,氮氧化物在北方泥炭地和森林中的沉积将增加,因此,氮氧化物排放源的增加。增加的氮沉积物可能会影响泥炭地植物区系,并改变泥炭地中的氮循环模式,因此,有必要研究这些效应在多少水平的过量氮沉积中发生。本文讨论了在加拿大艾伯塔省东北部马里亚纳湖小村庄附近的一个泥炭地综合体进行的为期5年的氮肥研究的前两年的结果,旨在量化这些泥炭地生态系统的氮“临界负荷”。在研究地点,有42个试验地块-一半在营养养护的沼泽中,另一半在贫瘠的沼泽中-氮肥的施用量从0公斤/公顷/年到25公斤/公顷/年不等。为了调查马里亚纳湖研究地点的植物对氮的吸收,我测量了泥炭天花组织和维管植物叶组织的氮(N)和碳(C)浓度。对于泥炭藓属物种,我还分析了C:N比和首字母N含量。为了研究目标泥炭藓种的潜在生长响应,需要进行线性生长(泥炭茎芽的垂直伸长),茎质量密度(泥炭茎去除鳞茎后,泥炭茎的重量占一定体积)的测量,最后测量净初级生产(前两次测量的乘积)。还测量了头皮质量密度(生物量),以研究泥炭藓头皮生长的可能变化。另外,在生长季节的高峰期(2011年7月中旬和2012年),对每个处理区的植物群落进行了采样,以提供“基准”数据,以记录氮肥后可能发生的植物分布或群落组成的任何变化。补充。

著录项

  • 作者

    Petix, Meaghan.;

  • 作者单位

    Southern Illinois University at Carbondale.;

  • 授予单位 Southern Illinois University at Carbondale.;
  • 学科 Biology Botany.;Biology Ecology.
  • 学位 M.S.
  • 年度 2014
  • 页码 156 p.
  • 总页数 156
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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