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Spatial and temporal heterogeneity of nitrogen, carbon and vegetation in the Wisconsin River and its floodplain, Wisconsin, USA.

机译:美国威斯康星河及其漫滩平原中氮,碳和植被的时空异质性。

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摘要

Understanding the roles of spatial and temporal heterogeneity in ecosystems is a frontier in ecology. In fluvial systems, flow regime generates spatial and temporal heterogeneity, yet many ecological consequences of this heterogeneity are not well studied. I examined the role of flow regime and spatial heterogeneity on aspects of biogeochemical cycling, soil organic matter and vegetation in reaches of the Wisconsin River and its floodplain. Lateral connections between the river and floodplain are largely intact, but flow is highly regulated by mainstem dams. On vegetated and unvegetated riverine sandbars, I measured hyporheic water chemistry and potential denitrification in months with varying river flow rates. Vegetation did not facilitate potential denitrification in Wisconsin River sandbars, but unvegetated sandbars were hotspots of nitrate processing. Unvegetated sandbars shifted from nitrate sources to sinks as the hydrograph declined. However, nitrate sinks were more prominent in a high discharge year, while sources predominated in a low discharge year. Anthropogenic modifications to the flow regime result in reduced flood peaks, which may limit nitrogen retention in this system.; In the floodplain, I used geostatistics to analyze the spatial pattern and content of soil organic matter along a flood frequency gradient. In all floodplain sites, a cyclic spatial pattern of soil organic matter was present. These repeating patterns may be generated by microtopography, specifically by differences in litter composition between ridges and swales. Overbank flood events appeared not to affect sediment sorting across the flood frequency gradient.; Lastly, I assessed how flow regime, landscape configuration and landscape quality predicted the presence, abundance and productivity of invasive shrubs (Lonicera and Rhamnus spp. and the native Zanthoxylum americanum) in the floodplain. Habitat configuration and quality associated with forest edge habitats were important predictors of invasives. Flooding decreased the presence of Lonicera and Rhamnus, but flood frequency increased the presence, abundance and productivity Z. americanum. Invasives were more also frequent in reaches where flooding was restricted. Overall, my research indicates that flooding and anthropogenic modifications to flow regimes influence spatial and temporal patterns of biogeochemical cycling, soils, and vegetation patterns in river-floodplain ecosystems.
机译:理解空间和时间异质性在生态系统中的作用是生态学的前沿。在河流系统中,流动状态会产生时空异质性,但是对这种异质性的许多生态后果还没有很好的研究。我研究了流态和空间异质性在威斯康星河及其洪泛区的生物地球化学循环,土壤有机质和植被方面的作用。河流和洪泛区之间的横向连接基本完好无损,但流量受到主干水坝的高度调节。在无植被和无植被的河道沙洲上,我测量了河水流量变化情况下数月的低水化学性质和潜在的反硝化作用。威斯康星河沙洲的植被没有促进潜在的反硝化作用,但是无植被的沙洲是硝酸盐加工的热点。随着水位线的下降,无植被的沙洲从硝酸盐源转变为汇。但是,硝酸盐汇在高排放年更为突出,而氮源在低排放年占主导地位。人为改变流态会导致洪峰减少,这可能会限制系统中的氮滞留。在洪泛区,我使用地统计学方法分析了洪水频率梯度下土壤有机质的空间格局和含量。在所有洪泛区,土壤有机质都有周期性的空间格局。这些重复的图案可以通过微形貌,特别是通过脊和大ale之间的凋落物组成的差异来产生。堤岸洪水事件似乎并未影响整个洪水频率梯度上的泥沙分类。最后,我评估了水流状况,景观配置和景观质量如何预测泛滥平原中入侵灌木(忍冬属植物和忍冬属植物和美洲花椒)的存在,丰度和生产力。与森林边缘生境相关的生境配置和质量是入侵物的重要预测因子。洪水减少了忍冬和鼠李的存在,但洪水频率增加了美洲忍冬的存在,丰度和生产力。在洪水泛滥的地区,入侵者也更为频繁。总的来说,我的研究表明,洪水和人为改变流态会影响河漫滩生态系统中生物地球化学循环的时空格局,土壤和植被格局。

著录项

  • 作者

    Predick, Katharine I.;

  • 作者单位

    The University of Wisconsin - Madison.;

  • 授予单位 The University of Wisconsin - Madison.;
  • 学科 Biology Ecology.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 112 p.
  • 总页数 112
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 生态学(生物生态学);
  • 关键词

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