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Nitrogen-use-efficiency in Sphagnum mosses: Effects of atmospheric nitrogen deposition.

机译:泥炭藓中的氮利用效率:大气氮沉积的影响。

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Sphagnum bogs are nutrient-poor ecosystems where plant growth is partly constrained by low nutrient levels. In these bogs, the entire water and nutrient supply is from atmospheric sources, such as precipitation, thus they are susceptible to changes in atmospheric chemistry. As atmospheric deposition of nitrogen increases from anthropogenic activity, it is likely that the Sphagnum mosses that dominate these bogs will be impacted directly. In this thesis, first I tested the hypothesis that Sphagnum nitrogen-use-efficiency decreases as nitrogen inputs from atmospheric deposition increase. I identified nitrogen retention from precipitation and internal nitrogen translocation as two key mechanisms for maximizing nitrogen-use-efficiency in Sphagna. I compared Sphagnum mosses in a high nitrogen deposition region in New York, to a low deposition region in Maine. I applied an 15N tracer to Sphagna in both regions, and estimated nitrogen retention and translocation.; Nitrogen retention ranged from 50% to 90%, and translocation ranged from 11% to 80% of nitrogen applied. Contrary to my hypothesis, both nitrogen retention and translocation appeared to be controlled more by climate and position of the water table rather than historical and recent nitrogen loads from atmospheric deposition. Further, these data suggest that nitrogen retention and translocation play equal roles in the Sphagnum nitrogen budget, each contributing approximately 10% of required nitrogen. Mineralization is likely an important sources to support Sphagnum nitrogen requirements.; Second, I proposed and tested a conceptual model of Sphagnum responses to increased atmospheric nitrogen deposition. The model included changes in tissue nitrogen concentrations and net primary production (NPP) as key parameters, and I tested it using my own data and data collected from the literature. I found three phases of Sphagnum responses to atmospheric nitrogen deposition, with critical nitrogen loads for each phase. Tissue nitrogen concentrations increased linearly with nitrogen deposition in the first phase, leveled off in the second phase, and ultimately decreased in the third phase. At all levels of nitrogen deposition, NPP was more strongly predicted by climatic variables than by nitrogen deposition. Results from this thesis indicate significant impacts of nitrogen loading on the Sphagnum mosses, even at low levels of nitrogen deposition.
机译:泥炭藓沼泽是营养贫乏的生态系统,其中植物的生长部分受到低营养水平的限制。在这些沼泽中,全部的水和养分供应都来自大气来源,例如降水,因此它们容易受到大气化学变化的影响。随着人为活动增加了大气中氮的沉积,支配这些沼泽的苔藓很可能会受到直接影响。在本文中,我首先检验了以下假设:随着来自大气沉积的氮输入增加,<斜体>泥炭藓的氮利用效率降低。我确定了来自降水和内部氮转运的氮保留是最大化氮利用效率的两个关键机制。我将纽约州一个高氮沉积区与缅因州一个低沉积区的泥炭藓苔藓进行了比较。我在两个区域的 Sphagna 中都使用了 15 N示踪剂,并估算了氮的保留和转运。氮保留量为施用氮的50%至90%,易位程度为11%至80%。与我的假设相反,氮的保留和转运似乎更多地受气候和地下水位的控制,而不是历史和最近的大气沉积氮负荷所控制。此外,这些数据表明氮的保留和转运在氮预算中起着相同的作用,各自贡献了所需氮的10%。矿化可能是支持球茎氮需求的重要来源。其次,我提出并测试了泥炭藓对大气氮沉积增加的响应的概念模型。该模型包括组织氮浓度和净初级生产(NPP)的变化作为关键参数,我使用自己的数据和从文献中收集的数据对其进行了测试。我发现了泥炭藓对大气氮沉积的三个阶段,每个阶段都有临界氮负荷。组织氮浓度在第一阶段随氮的沉积而线性增加,在第二阶段趋于稳定,最后在第三阶段下降。在所有水平的氮沉降下,相比于氮沉降,气候变量更能预测NPP。该论文的结果表明,即使在低水平的氮沉降下,氮负荷对苔藓也具有显着影响。

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