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Lakes and forests as determinants of downstream nutrient concentrations in small mountain watersheds

机译:湖泊和森林是山区小流域下游营养素浓度的决定因素

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Lakes are dynamic processors of nutrients and may hold an active role in modifying the water chemistry of stream systems. In this study, we examine the influence of lakes and an important terrestrial component-forest cover-on the nutrient levels of stream water in 11 Rocky Mountain (Idaho) watersheds. Water samples were collected from the inflow and outflow of lakes with varying amounts of upstream lakes and forested area during spring runoff and summer base flow. During base flow, mean total nitrogen concentrations at the inflow of final lakes were significantly related to relative upstream lake area, increasing from 34 to 103 mu g N L-1 as upstream lake cover in the watersheds increased from 0% to 4%. Forest cover was not significantly correlated with total nitrogen concentrations exported from the watersheds. However, similar to other studies, inflow nitrate concentrations were negatively correlated with relative forest cover. At the scale of individual lakes, dissolved organic carbon and dissolved organic nitrogen increased, and nitrate was significantly reduced from inflows to outflows. The results indicate a potentially critical role of mountain lakes in governing nitrogen flux downstream, and suggest the role of lakes as nitrogen sinks or sources may reverse between spring runoff and summer base flow.
机译:湖泊是养分的动态加工者,并可能在改变河流系统的水化学性质方面发挥积极作用。在这项研究中,我们研究了11个落基山(爱达荷州)流域的湖泊和重要的陆地成分-森林覆盖对溪流水养分的影响。在春季径流和夏季基流期间,从湖泊的流入和流出中收集水样,其中上游湖泊和林区的数量各不相同。在基流期间,随着流域中上游湖泊的覆盖率从0%增加到4%,最终湖泊流入处的平均总氮浓度与上游上游湖泊面积显着相关,从34μgN L-1增加到103μgN L-1。森林覆盖与流域输出的总氮浓度没有显着相关。但是,与其他研究类似,硝酸盐流入量与相对森林覆盖率呈负相关。在单个湖泊的规模上,溶解的有机碳和溶解的有机氮增加,硝酸盐从流入量减少到流出量。结果表明,高山湖泊在控制下游氮通量方面可能发挥关键作用,并表明湖泊在春季径流和夏季基流之间作为氮汇或氮源的作用可能会逆转。

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